the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 18 Nov 2024
The 3D Qp Model of the China Seismic Experiment Site (CSES-Q1.0) and Its Tectonic Implications
Abstract. The Chuan-Dian region is located in the southeastern part of the geologically complex and seismically active Tibetan Plateau. Since 2008, the Chuan-Dian region has experienced several major earthquakes, including the Wenchuan MS 8.0, Lushan MS 7.0, and Jiuzhaigou MS7.0, making it one of the areas with the most severe earthquake disasters. The China Seismic Experimental Site (CSES) under construction in this area will deepen the understanding of the preparation and generation of earthquakes and the disaster mechanisms, which can further enhance the defense capability against earthquake risks. To build a world-class seismic experimental field, it is necessary to establish high-precision medium structure models. Currently, several institutions have established high-resolution three-dimensional (3D) velocity models in the CSES, but there is still a lack of high-resolution 3D attenuation (∝1/Q) structure models. Using the local seismic tomography method, we obtain the highest resolution 3D Qp model in the CSES to date. Combining the existing velocity models in the CSES with other geophysical and geochemical observations by predecessors, this study find that the Qp value anomalies along large fault zones and some basin areas are low, reflecting the high degree of medium fragmentation in these areas, with thick sedimentary layers or rich in fluids. The high attenuation anomaly of the upper crust dipping westward in the Tengchong volcanic characterizes the possible upward flow of deep-seated magma from west to east. This study also find that most of earthquakes above magnitude 6 occurred in low attenuation zones or the boundary areas of high-low attenuation anomalies. The source areas of the 2008 Wenchuan MS 8.0 earthquake and the 2013 Lushan MS 7.0 earthquake were separated by a low attenuation area, and there is still a risk of major earthquakes in the future. The 3D attenuation model constructed in this study will provide a high-resolution reference model for seismological and earthquake disaster research in the CSES.
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Status: closed
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RC1: 'Comment on egusphere-2024-3340', Anonymous Referee #1, 31 Dec 2024
Review Comments
This paper presents attenuation tomography of southwestern China using a large dataset, yielding an updated, high-resolution attenuation model that complements existing velocity models. The new model provides valuable insights into fault zone structures and seismic risk in the region. Overall, the manuscript is well written, and both the methodology and inversion results appear robust. My primary concerns pertain to the need for additional technical details and consideration of alternative explanations for the high-attenuation fault zones. These suggestions do not require new tests or experiments and can likely be addressed with minor revisions. Please see the detailed comments below:
- While Q tomography is a well-established method, a more comprehensive description of the method would benefit this paper. In particular, please elaborate on the spectrum-fitting algorithm, the kernel construction, and the formulation of the inverse problem to ensure readers can fully understand your approach.
- From my own experience with Lg-wave attenuation, Q measurements can be sensitive to the frequency spectrum characteristics (e.g., spectrum holes) and the chosen fitting algorithm. Hence, some quality control may be required to preserve reliable measurements. I suggest showing the distribution of t* measurements as a function of distance, which may help to detect any potential systematic patterns or outliers.
- For the low-Q anomalies along major fault zones (e.g., LMSF, XJF), fluid-related attenuation is undoubtedly a key factor. However, scattering attenuation can also contribute to seismic energy loss, especially in complex, fragmented fault zones following large earthquakes. Please consider exploring scattering as an alternative or additional explanation for these observations.
Minor Comments
Figure 2: Consider using density plots to illustrate the distribution of earthquakes before and after declustering.
Line 119: Please clarify why a threshold value of 2.56 was selected.
Line 124: Provide more details on the “iterative algorithm” used for spectrum fitting.
Line 145: Explain how the weight varies with epicentral distance and, if possible, include a comparison of the data misfit distribution between the initial and final models.
Line 150: Change “Add 5%” to “We add 5%.”
Figure 4: Show the major fault zones on the checkerboard plot as well, and consider adding markers (e.g., circles) for key cities/towns.
Lines 166–167: The resolution matrix has not been introduced in previous sections. Please add an explanation of the inversion process and the role of the resolution matrix in the methodology section.
Line 170: Correct the typo “fixe” to “fix.”
Line 239: Replace “Wu et al. (2024)” with the model name “CSES-VM1.0.”
Line 272: For heat flow units (mW/m²), ensure the square is properly subscripted.
Line 344: Change “prepare strong earthquakes” to “host strong earthquakes.”
Line 351: Change “means” to “suggests.”
Citation: https://doi.org/10.5194/egusphere-2024-3340-RC1 -
AC1: 'Reply on RC1', Lianqing Zhou, 27 Feb 2025
Review Comments
Reviewer #1
1. This paper presents attenuation tomography of southwestern China using a large dataset, yielding an updated, high-resolution attenuation model that complements existing velocity models. The new model provides valuable insights into fault zone structures and seismic risk in the region. Overall, the manuscript is well written, and both the methodology and inversion results appear robust. My primary concerns pertain to the need for additional technical details and consideration of alternative explanations for the high-attenuation fault zones. These suggestions do not require new tests or experiments and can likely be addressed with minor revisions. Please see the detailed comments below:
While Q tomography is a well-established method, a more comprehensive description of the method would benefit this paper. In particular, please elaborate on the spectrum-fitting algorithm, the kernel construction, and the formulation of the inverse problem to ensure readers can fully understand your approach.
R. According to your suggestion, we have added the spectrum-fitting algorithm, the kernel construction, and the formulation of the inverse problem in the revisied manuscript. It should be noted that in the original text, "the fit values with the fitting error less than 0.1 s, 0.2 s, 0.3 s and 0.4 s" should be changed to "0.1, 0.2, 0.3, 0.4," without units. We have incorporated the above explanations into the revised manuscript. Please see “2 Method”section in the revised manuscript.
2. From my own experience with Lg-wave attenuation, Q measurements can be sensitive to the frequency spectrum characteristics (e.g., spectrum holes) and the chosen fitting algorithm. Hence, some quality control may be required to preserve reliable measurements. I suggest showing the distribution of t* measurements as a function of distance, which may help to detect any potential systematic patterns or outliers.
R. We agree with your opinion, Q value does have frequency dependence. We assume frequency independent attenuation in this paper. Studies that solve for 3-D Q with a range of α find that the resulting Q models are similar and equivalent in terms of interpreting Q structure (Lees & Lindley, 1994). Eberhart-Phillips & Chadwick (2002) believed that over the typical usable frequency range of their observations a frequency dependence of 0.3 would make < 10% difference in the amplitude decay compared to frequency independence. Eberhart-Phillips et al. (2014) tested different frequency-dependent factors (α = 1-0.6), they found that most spectra have equivalent fit with or without frequency dependence, and a small proportion favor either α = 0 or α = 0.4-0.6. Thus, they cannot determine that frequency dependence is necessary. Because of most other studies believe that α = 0.5, and thus they use 0.5 for comparison of frequency-dependent Q and found a strong linear relation. Hence 3-D Q models would have similar patterns for α = 0 and α = 0.5, and they choose to obtain frequency independent 3-D Q models. Therefore, we believe that the frequency independence Q values may be higher, but the medium characteristics revealed by it will be not change much.
To obtain high-quality t∗ data, we conducted quality control in the following ways:
Testing the fitting frequency band: By testing different fitting frequency bands, we ultimately selected the2-20 Hz band as the t∗fitting frequency band to obtain more high-quality t∗
Weighting t∗based on fitting error: We discardedt∗data with fitting errors greater than 0.4 while ensuring that each event had at least three t∗data points.
Removing unreliable t∗data: During the inversion of Qvalues, the program automatically discarded unreliable t∗data with Q>1500.
Assigning different weights to epicentral distances: During inversion, we weighted t∗data from different epicentral distances to further leverage the role of near-field stations in the inversion process.
Testing the impact of velocity models: Our previous studies have also discussed that the impact of velocity models on Qvalue inversion is minimal (Duan et al., 2024).
3. For the low-Q anomalies along major fault zones (e.g., LMSF, XJF), fluid-related attenuation is undoubtedly a key factor. However, scattering attenuation can also contribute to seismic energy loss, especially in complex, fragmented fault zones following large earthquakes. Please consider exploring scattering as an alternative or additional explanation for these observations.
R. Thank you for your suggestion.The main rupture of the Wenchuan earthquake occurred near Yingxiu on the Beichuan Fault, with both the Beichuan Fault and the Pengguan Fault experiencing severe ruptures, with rupture lengths reaching 240–300 km and ~90 km, respectively (Zhang et al., 2009a). These two major earthquakes have significantly fragmented the medium along the Longmenshan Fault. Additionally, a series of complex rock bodies (757–805 Ma) are exposed along the Longmenshan Fault from north to south, including the Nanba Complex, Pengguan Complex, Baoxing Complex, and Kangding Complex (Zhang et al., 2009b). Therefore, the high attenuation anomaly may partly reflect strong medium inhomogeneity, leading to scattering attenuation.XJF has experienced multiple tectonic movements, with acidic and basic magmatic intrusions during the Jinning, Caledonian, and Hercynian periods, causing large amounts of basalt and ultrabasic rock bodies to be exposed along the fault (Li, 1993). The high attenuation observed along the fault may also be due to scattering attenuation caused by the inhomogeneity of these unconsolidated rocks.
We added some explanation for scattering attenuation along LMSF and XJF. Please see “4.1 Spatial distribution characteristics of media structure in typical structural areas” section in the revised manuscript.
Minor Comments
4. Figure 2: Consider using density plots to illustrate the distribution of earthquakes before and after declustering.
R. Corrected.
5. Line 119: Please clarify why a threshold value of 2.56 was selected.
R. We have referenced several studies.They show that traditional methods of t*estimation often used the fixed time window such as 2.56s after the P-wave onset to calculate the observed velocity spectra of P waves and fit t* (Lees & Lindley1994; Eberhart-Phillips & Chadwick 2002; Hauksson & Shearer, 2006). Some earthquakes have epicentral distances of less than 20 km, and the S-P traveltime differences are less than 2.56 s. For these closer stations, the window length for the recorded P-wave is set to the S-P traveltime differences.
6. Line 124: Provide more details on the “iterative algorithm” used for spectrum fitting.
R. Please refer to the response to the first question.
7. Line 145: Explain how the weight varies with epicentral distance and, if possible, include a comparison of the data misfit distribution between the initial and final models.
R. During the inversion,t* data withhypocentral distances less than 50 km were weighted by a factor of 1, and t* data with hypocentral distances between 50 and 200 km were weighted by a linear function between 1 and 0, and t* data with hypocentral distances larger than 200 km were discarded. After 6 iterations, the final data variance of QP inversion decreased from 00054 to 0.000294, a reducation of 46% compared with the first inversion.
8. Line 150: Change “Add 5%” to “We add 5%.”
R. Corrected.
9. Figure 4: Show the major fault zones on the checkerboard plot as well, and consider adding markers (e.g., circles) for key cities/towns.
R. Corrected.
10. Lines 166–167: The resolution matrix has not been introduced in previous sections. Please add an explanation of the inversion process and the role of the resolution matrix in the methodology section.
R. We have added the explanation in the manuscript. The revised inversion process also described in the Methods section.
11. Line 170: Correct the typo “fixe” to “fix.”
R. Corrected.
12. Line 239: Replace “Wu et al. (2024)” with the model name “CSES-VM1.0.”
R. Corrected.
13. Line 272: For heat flow units (mW/m²), ensure the square is properly subscripted.
R. The heat flow unitsare right.
14. Line 344: Change “prepare strong earthquakes” to “host strong earthquakes.”
R. Corrected.
15. Line 351: Change “means” to “suggests.”
R. Corrected.
References
Duan, M., L. Zhou, C. Zhao, Z. Liu, and X. Zhang (2024). High-Resolution 3D QP and QS Models of the Middle Eastern Boundary of the Sichuan–Yunnan Rhombic Block: New Insight into Implication for Seismogenesis, Seismol. Res. Lett., doi: 10.1785/0220230232.
Hauksson, E., and P. M. Shearer (2006). Attenuation models (Qp and Qs) in three dimensions of the southern California crust : Inferred fluid saturation at seismogenic depths, J. Geophys. Res.-Solid Earth 111, no. B5, B05302–B05322, doi: 10.1029/2005JB003947.
Lees, J. M., and G. T. Lindley (1994). Three-dimensional attenuation tomography at Loma Prieta: Inversion of t* for Q, J. Geophys. Res.-Solid Earth 99, no. B4, 6843–6863, doi: 10.1029/93JB03460.
Li, P. (1993). The Xianshuihe-Xiaojiang fault zone [M]. Seismological Press, Beijing (in Chinese).
Zhang, Y., W. P. Feng, L. S. Xu, C. H. Zhou and Y. T. Chen (2009a). Spatio-temporal rupture process of the 2008 great Wenchuan earthquake, Sci. China Earth Sci., 52 (2):145-154. https://doi.org/10.1007/s11430-008-0148-7.
Zhang. Z., Y. Wang, Y. Chen, et al. (2009b). Crustal structure across Longmenshan fault belt from passive source seismic profiling. Geophys. Res. Lett., 36.
Citation: https://doi.org/10.5194/egusphere-2024-3340-AC1
-
RC2: 'Comment on egusphere-2024-3340', Shaolin Liu, 25 Feb 2025
The manuscript presents a high-resolution 3D Qp model for the China Seismic Experiment Site (CSES) and provides valuable insights into the tectonic implications of attenuation structures. The study is methodologically sound, well-structured, and addresses a critical gap in seismic attenuation modeling for this seismically active region. The integration of velocity models, geochemical observations, and geological data strengthens the conclusions. I think this is a good study and their interpretations are reasonable to me. As far as I understand, the model proposed in this article is currently the first high-resolution attenuation model in the Sichuan-Yunnan region and is recommended as a public model for the China Earthquake Science Experiment Field. The manuscript is otherwise well-prepared and merits publication in Solid Earth after minor revisions.
Minor Revisions:
1. It is more appropriate to change CSES-Q1.0 to CSESQ-V1.0 in the title.
2. Minor grammatical inconsistencies exist (e.g., "layed" in Figure 4 caption should be "layered"). A thorough proofread is recommended.
3. L97: Clarify earthquakes with at least six phases" means six P phases or both P and S phases?
4. Please provide additional details of SIMUL2000 parameters on damping factor and weight setting in section 2.2.
5. Standardize journal abbreviations (e.g., "Geophys. J. Int." vs. "Geophys J Int", "J. Geophys. Res. Solid Earth" vs "J. Geophys. Res.-Solid Earth" and "J. Geophys. Res.").
6. Figure 2 appears relatively blurry, and the distinction between earthquakes in (a) and (b) is not very clear. It is recommended to represent the earthquakes with hollow circles or solid circles with borders, and upload a vector image.
7. Figure 3 and 4 are also not very clear, please upload vector images.
8. The labels of the legend in Figure 5 are not seperated, please correct them.
9. Change "Spread_Fuction" to "Spread Function" in Figure 6.Citation: https://doi.org/10.5194/egusphere-2024-3340-RC2 -
AC2: 'Reply on RC2', Lianqing Zhou, 27 Feb 2025
Reviewer #2
The manuscript presents a high-resolution 3D Qp model for the China Seismic Experiment Site (CSES) and provides valuable insights into the tectonic implications of attenuation structures. The study is methodologically sound, well-structured, and addresses a critical gap in seismic attenuation modeling for this seismically active region. The integration of velocity models, geochemical observations, and geological data strengthens the conclusions. I think this is a good study and their interpretations are reasonable to me. As far as I understand, the model proposed in this article is currently the first high-resolution attenuation model in the Sichuan-Yunnan region and is recommended as a public model for the China Earthquake Science Experiment Field. The manuscript is otherwise well-prepared and merits publication in Solid Earth after minor revisions.
Minor Revisions:
1. It is more appropriate to change CSES-Q1.0 to CSESQ-V1.0 in the title.
R. Thank you for your suggestions. Considering that CSES is a proprietary abbreviation for the China Seismic Experimental Site, combining it with Qmight not be easily recognizable. Since V can be easily misinterpreted as Velocity, to avoid confusion, we prefer to retain the abbreviation CSES-Q1.0.
2. Minor grammatical inconsistencies exist (e.g., "layed" in Figure 4 caption should be "layered"). A thorough proofread is recommended.
R. Corrected.3. L97: Clarify earthquakes with at least six phases" means six P phases or both P and S phases?
R. It means six both P and S phases.
4. Please provide additional details of SIMUL2000 parameters on damping factor and weight setting in section 2.2.
R. Weset maximum number of iterations to 10 to perform inversions with Qvalues between 50 and 650. According to the minimum value of data variance, the initial values of QP was set to 350 with 9 iterations. Then, according to the trade-off curve between the model variance and the data variance from the inversion with a single iteration, the optimal damping values of QP tomography was set to 0.1. We have added the details in the manuscript.
5. Standardize journal abbreviations (e.g., "Geophys. J. Int." vs. "Geophys J Int", "J. Geophys. Res. Solid Earth" vs "J. Geophys. Res.-Solid Earth" and "J. Geophys. Res.").
R. Corrected.
6. Figure 2 appears relatively blurry, and the distinction between earthquakes in (a) and (b) is not very clear. It is recommended to represent the earthquakes with hollow circles or solid circles with borders, and upload a vector image.
R. In accordance with the suggestions of Reviewer 1, we usedensity plots to illustrate the distribution of earthquakes before and after declustering.7. Figure 3 and 4 are also not very clear, please upload vector images.
R. Wehave uploaded the vector images of the two figures.8. The labels of the legend in Figure 5 are not seperated, please correct them.
R. Corrected.
9. Change "Spread_Fuction" to "Spread Function" in Figure 6.
R. Corrected.Citation: https://doi.org/10.5194/egusphere-2024-3340-AC2
-
AC2: 'Reply on RC2', Lianqing Zhou, 27 Feb 2025
Status: closed
-
RC1: 'Comment on egusphere-2024-3340', Anonymous Referee #1, 31 Dec 2024
Review Comments
This paper presents attenuation tomography of southwestern China using a large dataset, yielding an updated, high-resolution attenuation model that complements existing velocity models. The new model provides valuable insights into fault zone structures and seismic risk in the region. Overall, the manuscript is well written, and both the methodology and inversion results appear robust. My primary concerns pertain to the need for additional technical details and consideration of alternative explanations for the high-attenuation fault zones. These suggestions do not require new tests or experiments and can likely be addressed with minor revisions. Please see the detailed comments below:
- While Q tomography is a well-established method, a more comprehensive description of the method would benefit this paper. In particular, please elaborate on the spectrum-fitting algorithm, the kernel construction, and the formulation of the inverse problem to ensure readers can fully understand your approach.
- From my own experience with Lg-wave attenuation, Q measurements can be sensitive to the frequency spectrum characteristics (e.g., spectrum holes) and the chosen fitting algorithm. Hence, some quality control may be required to preserve reliable measurements. I suggest showing the distribution of t* measurements as a function of distance, which may help to detect any potential systematic patterns or outliers.
- For the low-Q anomalies along major fault zones (e.g., LMSF, XJF), fluid-related attenuation is undoubtedly a key factor. However, scattering attenuation can also contribute to seismic energy loss, especially in complex, fragmented fault zones following large earthquakes. Please consider exploring scattering as an alternative or additional explanation for these observations.
Minor Comments
Figure 2: Consider using density plots to illustrate the distribution of earthquakes before and after declustering.
Line 119: Please clarify why a threshold value of 2.56 was selected.
Line 124: Provide more details on the “iterative algorithm” used for spectrum fitting.
Line 145: Explain how the weight varies with epicentral distance and, if possible, include a comparison of the data misfit distribution between the initial and final models.
Line 150: Change “Add 5%” to “We add 5%.”
Figure 4: Show the major fault zones on the checkerboard plot as well, and consider adding markers (e.g., circles) for key cities/towns.
Lines 166–167: The resolution matrix has not been introduced in previous sections. Please add an explanation of the inversion process and the role of the resolution matrix in the methodology section.
Line 170: Correct the typo “fixe” to “fix.”
Line 239: Replace “Wu et al. (2024)” with the model name “CSES-VM1.0.”
Line 272: For heat flow units (mW/m²), ensure the square is properly subscripted.
Line 344: Change “prepare strong earthquakes” to “host strong earthquakes.”
Line 351: Change “means” to “suggests.”
Citation: https://doi.org/10.5194/egusphere-2024-3340-RC1 -
AC1: 'Reply on RC1', Lianqing Zhou, 27 Feb 2025
Review Comments
Reviewer #1
1. This paper presents attenuation tomography of southwestern China using a large dataset, yielding an updated, high-resolution attenuation model that complements existing velocity models. The new model provides valuable insights into fault zone structures and seismic risk in the region. Overall, the manuscript is well written, and both the methodology and inversion results appear robust. My primary concerns pertain to the need for additional technical details and consideration of alternative explanations for the high-attenuation fault zones. These suggestions do not require new tests or experiments and can likely be addressed with minor revisions. Please see the detailed comments below:
While Q tomography is a well-established method, a more comprehensive description of the method would benefit this paper. In particular, please elaborate on the spectrum-fitting algorithm, the kernel construction, and the formulation of the inverse problem to ensure readers can fully understand your approach.
R. According to your suggestion, we have added the spectrum-fitting algorithm, the kernel construction, and the formulation of the inverse problem in the revisied manuscript. It should be noted that in the original text, "the fit values with the fitting error less than 0.1 s, 0.2 s, 0.3 s and 0.4 s" should be changed to "0.1, 0.2, 0.3, 0.4," without units. We have incorporated the above explanations into the revised manuscript. Please see “2 Method”section in the revised manuscript.
2. From my own experience with Lg-wave attenuation, Q measurements can be sensitive to the frequency spectrum characteristics (e.g., spectrum holes) and the chosen fitting algorithm. Hence, some quality control may be required to preserve reliable measurements. I suggest showing the distribution of t* measurements as a function of distance, which may help to detect any potential systematic patterns or outliers.
R. We agree with your opinion, Q value does have frequency dependence. We assume frequency independent attenuation in this paper. Studies that solve for 3-D Q with a range of α find that the resulting Q models are similar and equivalent in terms of interpreting Q structure (Lees & Lindley, 1994). Eberhart-Phillips & Chadwick (2002) believed that over the typical usable frequency range of their observations a frequency dependence of 0.3 would make < 10% difference in the amplitude decay compared to frequency independence. Eberhart-Phillips et al. (2014) tested different frequency-dependent factors (α = 1-0.6), they found that most spectra have equivalent fit with or without frequency dependence, and a small proportion favor either α = 0 or α = 0.4-0.6. Thus, they cannot determine that frequency dependence is necessary. Because of most other studies believe that α = 0.5, and thus they use 0.5 for comparison of frequency-dependent Q and found a strong linear relation. Hence 3-D Q models would have similar patterns for α = 0 and α = 0.5, and they choose to obtain frequency independent 3-D Q models. Therefore, we believe that the frequency independence Q values may be higher, but the medium characteristics revealed by it will be not change much.
To obtain high-quality t∗ data, we conducted quality control in the following ways:
Testing the fitting frequency band: By testing different fitting frequency bands, we ultimately selected the2-20 Hz band as the t∗fitting frequency band to obtain more high-quality t∗
Weighting t∗based on fitting error: We discardedt∗data with fitting errors greater than 0.4 while ensuring that each event had at least three t∗data points.
Removing unreliable t∗data: During the inversion of Qvalues, the program automatically discarded unreliable t∗data with Q>1500.
Assigning different weights to epicentral distances: During inversion, we weighted t∗data from different epicentral distances to further leverage the role of near-field stations in the inversion process.
Testing the impact of velocity models: Our previous studies have also discussed that the impact of velocity models on Qvalue inversion is minimal (Duan et al., 2024).
3. For the low-Q anomalies along major fault zones (e.g., LMSF, XJF), fluid-related attenuation is undoubtedly a key factor. However, scattering attenuation can also contribute to seismic energy loss, especially in complex, fragmented fault zones following large earthquakes. Please consider exploring scattering as an alternative or additional explanation for these observations.
R. Thank you for your suggestion.The main rupture of the Wenchuan earthquake occurred near Yingxiu on the Beichuan Fault, with both the Beichuan Fault and the Pengguan Fault experiencing severe ruptures, with rupture lengths reaching 240–300 km and ~90 km, respectively (Zhang et al., 2009a). These two major earthquakes have significantly fragmented the medium along the Longmenshan Fault. Additionally, a series of complex rock bodies (757–805 Ma) are exposed along the Longmenshan Fault from north to south, including the Nanba Complex, Pengguan Complex, Baoxing Complex, and Kangding Complex (Zhang et al., 2009b). Therefore, the high attenuation anomaly may partly reflect strong medium inhomogeneity, leading to scattering attenuation.XJF has experienced multiple tectonic movements, with acidic and basic magmatic intrusions during the Jinning, Caledonian, and Hercynian periods, causing large amounts of basalt and ultrabasic rock bodies to be exposed along the fault (Li, 1993). The high attenuation observed along the fault may also be due to scattering attenuation caused by the inhomogeneity of these unconsolidated rocks.
We added some explanation for scattering attenuation along LMSF and XJF. Please see “4.1 Spatial distribution characteristics of media structure in typical structural areas” section in the revised manuscript.
Minor Comments
4. Figure 2: Consider using density plots to illustrate the distribution of earthquakes before and after declustering.
R. Corrected.
5. Line 119: Please clarify why a threshold value of 2.56 was selected.
R. We have referenced several studies.They show that traditional methods of t*estimation often used the fixed time window such as 2.56s after the P-wave onset to calculate the observed velocity spectra of P waves and fit t* (Lees & Lindley1994; Eberhart-Phillips & Chadwick 2002; Hauksson & Shearer, 2006). Some earthquakes have epicentral distances of less than 20 km, and the S-P traveltime differences are less than 2.56 s. For these closer stations, the window length for the recorded P-wave is set to the S-P traveltime differences.
6. Line 124: Provide more details on the “iterative algorithm” used for spectrum fitting.
R. Please refer to the response to the first question.
7. Line 145: Explain how the weight varies with epicentral distance and, if possible, include a comparison of the data misfit distribution between the initial and final models.
R. During the inversion,t* data withhypocentral distances less than 50 km were weighted by a factor of 1, and t* data with hypocentral distances between 50 and 200 km were weighted by a linear function between 1 and 0, and t* data with hypocentral distances larger than 200 km were discarded. After 6 iterations, the final data variance of QP inversion decreased from 00054 to 0.000294, a reducation of 46% compared with the first inversion.
8. Line 150: Change “Add 5%” to “We add 5%.”
R. Corrected.
9. Figure 4: Show the major fault zones on the checkerboard plot as well, and consider adding markers (e.g., circles) for key cities/towns.
R. Corrected.
10. Lines 166–167: The resolution matrix has not been introduced in previous sections. Please add an explanation of the inversion process and the role of the resolution matrix in the methodology section.
R. We have added the explanation in the manuscript. The revised inversion process also described in the Methods section.
11. Line 170: Correct the typo “fixe” to “fix.”
R. Corrected.
12. Line 239: Replace “Wu et al. (2024)” with the model name “CSES-VM1.0.”
R. Corrected.
13. Line 272: For heat flow units (mW/m²), ensure the square is properly subscripted.
R. The heat flow unitsare right.
14. Line 344: Change “prepare strong earthquakes” to “host strong earthquakes.”
R. Corrected.
15. Line 351: Change “means” to “suggests.”
R. Corrected.
References
Duan, M., L. Zhou, C. Zhao, Z. Liu, and X. Zhang (2024). High-Resolution 3D QP and QS Models of the Middle Eastern Boundary of the Sichuan–Yunnan Rhombic Block: New Insight into Implication for Seismogenesis, Seismol. Res. Lett., doi: 10.1785/0220230232.
Hauksson, E., and P. M. Shearer (2006). Attenuation models (Qp and Qs) in three dimensions of the southern California crust : Inferred fluid saturation at seismogenic depths, J. Geophys. Res.-Solid Earth 111, no. B5, B05302–B05322, doi: 10.1029/2005JB003947.
Lees, J. M., and G. T. Lindley (1994). Three-dimensional attenuation tomography at Loma Prieta: Inversion of t* for Q, J. Geophys. Res.-Solid Earth 99, no. B4, 6843–6863, doi: 10.1029/93JB03460.
Li, P. (1993). The Xianshuihe-Xiaojiang fault zone [M]. Seismological Press, Beijing (in Chinese).
Zhang, Y., W. P. Feng, L. S. Xu, C. H. Zhou and Y. T. Chen (2009a). Spatio-temporal rupture process of the 2008 great Wenchuan earthquake, Sci. China Earth Sci., 52 (2):145-154. https://doi.org/10.1007/s11430-008-0148-7.
Zhang. Z., Y. Wang, Y. Chen, et al. (2009b). Crustal structure across Longmenshan fault belt from passive source seismic profiling. Geophys. Res. Lett., 36.
Citation: https://doi.org/10.5194/egusphere-2024-3340-AC1
-
RC2: 'Comment on egusphere-2024-3340', Shaolin Liu, 25 Feb 2025
The manuscript presents a high-resolution 3D Qp model for the China Seismic Experiment Site (CSES) and provides valuable insights into the tectonic implications of attenuation structures. The study is methodologically sound, well-structured, and addresses a critical gap in seismic attenuation modeling for this seismically active region. The integration of velocity models, geochemical observations, and geological data strengthens the conclusions. I think this is a good study and their interpretations are reasonable to me. As far as I understand, the model proposed in this article is currently the first high-resolution attenuation model in the Sichuan-Yunnan region and is recommended as a public model for the China Earthquake Science Experiment Field. The manuscript is otherwise well-prepared and merits publication in Solid Earth after minor revisions.
Minor Revisions:
1. It is more appropriate to change CSES-Q1.0 to CSESQ-V1.0 in the title.
2. Minor grammatical inconsistencies exist (e.g., "layed" in Figure 4 caption should be "layered"). A thorough proofread is recommended.
3. L97: Clarify earthquakes with at least six phases" means six P phases or both P and S phases?
4. Please provide additional details of SIMUL2000 parameters on damping factor and weight setting in section 2.2.
5. Standardize journal abbreviations (e.g., "Geophys. J. Int." vs. "Geophys J Int", "J. Geophys. Res. Solid Earth" vs "J. Geophys. Res.-Solid Earth" and "J. Geophys. Res.").
6. Figure 2 appears relatively blurry, and the distinction between earthquakes in (a) and (b) is not very clear. It is recommended to represent the earthquakes with hollow circles or solid circles with borders, and upload a vector image.
7. Figure 3 and 4 are also not very clear, please upload vector images.
8. The labels of the legend in Figure 5 are not seperated, please correct them.
9. Change "Spread_Fuction" to "Spread Function" in Figure 6.Citation: https://doi.org/10.5194/egusphere-2024-3340-RC2 -
AC2: 'Reply on RC2', Lianqing Zhou, 27 Feb 2025
Reviewer #2
The manuscript presents a high-resolution 3D Qp model for the China Seismic Experiment Site (CSES) and provides valuable insights into the tectonic implications of attenuation structures. The study is methodologically sound, well-structured, and addresses a critical gap in seismic attenuation modeling for this seismically active region. The integration of velocity models, geochemical observations, and geological data strengthens the conclusions. I think this is a good study and their interpretations are reasonable to me. As far as I understand, the model proposed in this article is currently the first high-resolution attenuation model in the Sichuan-Yunnan region and is recommended as a public model for the China Earthquake Science Experiment Field. The manuscript is otherwise well-prepared and merits publication in Solid Earth after minor revisions.
Minor Revisions:
1. It is more appropriate to change CSES-Q1.0 to CSESQ-V1.0 in the title.
R. Thank you for your suggestions. Considering that CSES is a proprietary abbreviation for the China Seismic Experimental Site, combining it with Qmight not be easily recognizable. Since V can be easily misinterpreted as Velocity, to avoid confusion, we prefer to retain the abbreviation CSES-Q1.0.
2. Minor grammatical inconsistencies exist (e.g., "layed" in Figure 4 caption should be "layered"). A thorough proofread is recommended.
R. Corrected.3. L97: Clarify earthquakes with at least six phases" means six P phases or both P and S phases?
R. It means six both P and S phases.
4. Please provide additional details of SIMUL2000 parameters on damping factor and weight setting in section 2.2.
R. Weset maximum number of iterations to 10 to perform inversions with Qvalues between 50 and 650. According to the minimum value of data variance, the initial values of QP was set to 350 with 9 iterations. Then, according to the trade-off curve between the model variance and the data variance from the inversion with a single iteration, the optimal damping values of QP tomography was set to 0.1. We have added the details in the manuscript.
5. Standardize journal abbreviations (e.g., "Geophys. J. Int." vs. "Geophys J Int", "J. Geophys. Res. Solid Earth" vs "J. Geophys. Res.-Solid Earth" and "J. Geophys. Res.").
R. Corrected.
6. Figure 2 appears relatively blurry, and the distinction between earthquakes in (a) and (b) is not very clear. It is recommended to represent the earthquakes with hollow circles or solid circles with borders, and upload a vector image.
R. In accordance with the suggestions of Reviewer 1, we usedensity plots to illustrate the distribution of earthquakes before and after declustering.7. Figure 3 and 4 are also not very clear, please upload vector images.
R. Wehave uploaded the vector images of the two figures.8. The labels of the legend in Figure 5 are not seperated, please correct them.
R. Corrected.
9. Change "Spread_Fuction" to "Spread Function" in Figure 6.
R. Corrected.Citation: https://doi.org/10.5194/egusphere-2024-3340-AC2
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AC2: 'Reply on RC2', Lianqing Zhou, 27 Feb 2025
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