Tingwei Yang, Tao Xu, Yinshuang Ai, Qingdong Zeng, Jinhui Yang, Laicheng Miao, Fan Zheng, Nanqiao Du
{"title":"Crustal Structure and its Control on Gold Mineralization in Wulong Goldfield, Liaodong Peninsula of China: Constraints from Ambient Noise Tomography with a Short-Period Dense Array","authors":"Tingwei Yang, Tao Xu, Yinshuang Ai, Qingdong Zeng, Jinhui Yang, Laicheng Miao, Fan Zheng, Nanqiao Du","doi":"10.1007/s00024-024-03554-5","DOIUrl":"10.1007/s00024-024-03554-5","url":null,"abstract":"<div><p>During the destruction of the North China Craton in the Mesozoic era, a significant gold mineralization event occurred, leading to the formation of the world-renowned Jiaodong Gold Province. The Liaodong and Jiaodong regions have similar tectonic backgrounds and geological evolution histories. However, the confirmed gold resources in the Liaodong region are only one-tenth of those in Jiaodong. To reveal the controlling factors behind the differences in mineralization between these two regions and explore the deep mineralization prospects in the Liaodong region, we conducted a short-period and high-density array (WSP array) in the Wulong Gold Concentrated Area, the largest goldfield in the Liaodong region. Using data recorded by 334 SmartSolo seismometers for one month, we applied ambient noise tomography to obtain the S-wave velocity structure of the crust down to a depth of 3.5 km beneath the Wulong goldfield. The velocity structure revealed the presence of two sets of low-velocity anomalies trending NNE and NW, respectively, in the shallow crust (shallower than 1.5 km) of the Wulong goldfield, while two high-velocity anomalies were identified at deeper depths (1.5–3.5 km). By combining these findings with the geological characteristics of the Wulong goldfield, it was discovered that the high-velocity anomaly (II) corresponds to the Sanguliu granitic body exposed at the surface, while the high-velocity anomaly (I) could be a concealed intrusive body. The shallow low-velocity anomalies are the result of hydrothermal alteration caused by mineralizing fluids along the NNE- and NW-trending faults. The intersection of these two sets of faults, where the low-velocity anomalies exist, represents the center of the hydrothermal activities. Based on these observations, it is proposed that the area between the Sanguliu granitic body and the concealed intrusive body in the northwest has favorable metallogenic conditions. The intersections of the NNE- and NW-trending faults show the high potential for forming large to super-large altered rock-type gold deposits.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 9","pages":"2973 - 2990"},"PeriodicalIF":1.9,"publicationDate":"2024-08-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142226669","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Anatol Guglielmi, Alexey Zavyalov, Oleg Zotov, Boris Klain
{"title":"The Omori Epoch: On the 100th Anniversary of the Death of a Famous Japanese Seismologist","authors":"Anatol Guglielmi, Alexey Zavyalov, Oleg Zotov, Boris Klain","doi":"10.1007/s00024-024-03560-7","DOIUrl":"10.1007/s00024-024-03560-7","url":null,"abstract":"<div><p>One hundred years ago, Fusakichi Omori died. Our paper is dedicated to his memory. Omori made an outstanding contribution to the physics of earthquakes. In 1894 he formulated the law of aftershock evolution. Omori’s Law states that after the main shock of an earthquake, the frequency of aftershocks decreases hyperbolically with time. In this paper, we briefly describe one of the directions of modern aftershock research. We present Omori’s law in the form of a differential equation describing the evolution of aftershocks. The evolution equation allows us to solve the inverse problem of the earthquake source “cooling down” after the main shock. The solution of the inverse problem allowed us to reveal the existence of the so-called Omori epoch. It is established that at the end of the Omori epoch something similar to a bifurcation of the source state occurs. A logistic equation supposedly describing the bifurcation phenomenon is proposed.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 9","pages":"2741 - 2752"},"PeriodicalIF":1.9,"publicationDate":"2024-08-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142209952","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Septriono Hari Nugroho, Purna Sulastya Putra, Amar, Mohammad Heidarzadeh
{"title":"Effects of Artificial Structures on Grain Size and Characteristics of the 2018 Anak Krakatau Tsunami Deposits","authors":"Septriono Hari Nugroho, Purna Sulastya Putra, Amar, Mohammad Heidarzadeh","doi":"10.1007/s00024-024-03558-1","DOIUrl":"10.1007/s00024-024-03558-1","url":null,"abstract":"<div><p>This paper presents the first detailed analysis of grain size parameters and tsunami deposit of the 2018 Anak Krakatau tsunami, considering artificial structures such as buildings and roads. The deposition of tsunamis on land is extremely complex, involving contributions from both the hydrodynamics of tsunami flow propagation and the characteristics of the tsunami, as well as topographical conditions. In both local and detailed contexts, artificial structures can affect the formation of tsunami deposits. In this study, we focused on the effect of artificial structures on the characteristics of the 2018 Anak Krakatau tsunami deposits. Field observations showed that the remains of dikes, houses and asphalt roads significantly influenced the source, thickness, structure of tsunami deposits and grain size parameters. Tsunami deposits consisting of fine-grained material originated from the sediment on the seafloor. Tsunami deposits were thicker in areas closer to the part of the sea unaffected by artificial structures and exhibited a thinning trend inland. In general, the grain size of tsunami deposits is coarser than that of pre-tsunami deposits. Tsunami deposits predominantly exhibit an upward fining trend. Our study explains the key role of artificial structures in the formation of tsunami deposits and the sediment structure produced in coastal areas. A drastic change in the characteristics of the grain size parameters results from the presence of artificial structures. Overall, the tsunami deposit layers could have been better sorted. Significantly different sortation values were observed at sites located above the asphalt road. Similarly, kurtosis values showed an anomaly. The skewness value was inversely proportional to the average grain size in areas affected by artificial structures.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 10","pages":"2991 - 3003"},"PeriodicalIF":1.9,"publicationDate":"2024-08-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142209910","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Ognjen Bonacci, Ana Žaknić-Ćatović, Tanja Roje-Bonacci, Stevan Prohaska, Duje Bonacci, Samir Ćatović
{"title":"Air and Water Temperature Trend Analysis at the Confluence of the Sava and Danube Rivers in Belgrade, Serbia","authors":"Ognjen Bonacci, Ana Žaknić-Ćatović, Tanja Roje-Bonacci, Stevan Prohaska, Duje Bonacci, Samir Ćatović","doi":"10.1007/s00024-024-03552-7","DOIUrl":"10.1007/s00024-024-03552-7","url":null,"abstract":"<div><p>This study highlights significant recent increases in water and air temperatures in the rapidly developing city of Belgrade, Serbia to raise awareness of the anticipated negative impacts and the urgent need to develop appropriate mitigation strategies. We investigate the mean annual water temperature trends at the confluence of the Sava and Danube Rivers, along with air temperature trends at the Belgrade meteorological station, spanning from 1956 to 2020. Results reveal a consistent increase in temperature across all three measuring stations, with the Danube experiencing a rise of 0.34 °C/decade, the Sava at 0.44 °C/decade, and Belgrade's air temperature increasing by 0.39 °C/decade. Employing the Rescaled Adjusted Partial Sums method, sharp rises in water temperature were pinpointed in 1989 for the Sava and 1990 for the Danube, while Belgrade's air temperature surge began in 1998. The highest intensity of air temperature increase within the recent period (1998–2020) was observed at the Belgrade observatory, reaching 0.76 °C/decade. Notably, the Sava exhibited a faster increase in water temperature over the last thirty years compared to the Danube. August marked the peak average water temperature for both rivers, while July recorded the highest average air temperature in Belgrade. Despite differing flow rates, both rivers exhibit similar hydrological regimes, with maximum flows occurring in April and minimum flows in August for the Sava, and October for the Danube. Seasonal temperature increases were most pronounced in summer, notably in August, with the smallest rises occurring during cold periods. Additionally, an inverse proportional relationship between mean annual water temperatures and discharges was observed at both river stations. The overall findings suggest that the increase in both air and water temperatures is more pronounced during the warmer part of the year.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 9","pages":"2895 - 2912"},"PeriodicalIF":1.9,"publicationDate":"2024-08-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s00024-024-03552-7.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142209911","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Prediction of Precipitation-Temperature Data and Drought Assessment of Turkey with Stochastic Time Series Models","authors":"Ahmet Iyad Ceyhunlu, Gokmen Ceribasi","doi":"10.1007/s00024-024-03559-0","DOIUrl":"10.1007/s00024-024-03559-0","url":null,"abstract":"<div><p>Throughout the geological history of Earth, there have been many changes in the climate system due to natural and external factors. In the past, it can be said that changes in climate were caused by natural causes, while today they are largely caused by human activities. Turkey is among the countries that will be affected by climate change. Therefore, In this study, a stochastic time series model was constructed to forecast the precipitation and temperature data of Turkey between 2020 and 2050. Seasonal Autoregressive Integrated Moving Average models were used to take into account the relationship between the data and seasonality factors. In addition, the most appropriate model for each station was established separately. The accuracy of the predicted data was tested by correlation test (r) and root mean square error (RMSE) test. As a result of the study, the average r value for temperature data was 99% and RMSE value was calculated as 1.46. For precipitation data, the average r value was calculated as 66% and RMSE value as 34.6. In addition, in this study, drought models for Turkey until 2050 were established and spatial and temporal evaluation of these models were made. These models were obtained by analyzing the data of uniformly distributed stations over Turkey between 1990 and 2050 with standard precipitation evapotranspiration index (SPEI). Different time scales (SPEI<sub>3</sub>, SPEI<sub>6</sub>, SPEI<sub>9</sub> and SPEI<sub>12</sub>) were used in drought analysis. As a result of this study, drought return interval maps of Turkey and drought maps between 1990 and 2050 were created.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 9","pages":"2913 - 2933"},"PeriodicalIF":1.9,"publicationDate":"2024-08-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142209931","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Rapid Moment Magnitude (Mwp) Calculation for UK Broadband Seismic Stations Using Teleseismic Waves","authors":"Timur Tezel, Gillian R. Foulger, Jon G. Gluyas","doi":"10.1007/s00024-024-03557-2","DOIUrl":"10.1007/s00024-024-03557-2","url":null,"abstract":"<div><p>Determining the magnitude of an earthquake rapidly and correctly is essential to starting simulations to evaluate the potential for tsunami generation and early warning for tsunami-prone countries and rapid response, considering countries that lie in seismically active regions. Although the UK does not have a high degree of tsunami hazard, the UK seismic network can estimate the moment magnitude for large earthquakes which will occur around the globe. This study aimed to test the UK Seismological Network Broadband Seismic Stations to calculate the P-wave moment magnitude (M<sub><b>wp</b></sub>) using teleseismic waves. The standard way to calculate the M<sub><b>wp</b></sub> is using the P-wave portion of a seismic wave recorded at different epicentral distances. We selected twenty-five seismic events with a magnitude greater than 6.5M<sub><b>w</b></sub> and epicentral distances between 17 and 90 degrees. The main issue is selecting the P-wave portion of a seismic wave and using a trial P-wave velocity to estimate the M<sub><b>wp</b></sub>. We simplified the selection of a P-wave portion of seismic waves using a theoretical formula that works with epicentral distance, P-wave arrival time and an apparent P-wave velocity, which calculates the S-wave arrival time. The results show the variation between the Harvard centroid moment tensor (CMT—M<sub><b>w</b></sub>) and M<sub><b>wp,</b></sub> which is about ± 0.1 magnitude units in most events and ± 0.2 for some events. These results prove the M<sub><b>wp</b></sub> technique can be applied to the UK broadband seismic network broadband seismic stations and encourage the use of it immediately following a destructive earthquake anywhere in the world.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 9","pages":"2753 - 2763"},"PeriodicalIF":1.9,"publicationDate":"2024-08-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142210099","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Hydro-meteorological Research Study in Madhya Pradesh, Central India: A Literature Review","authors":"Sarita Tiwari, Ashok Biswal, Gajanan Ramteke","doi":"10.1007/s00024-024-03553-6","DOIUrl":"10.1007/s00024-024-03553-6","url":null,"abstract":"<div><p>Water is a crucial and invaluable natural resource essential for humanity to sustain on Earth. Around 70% of the Earth’s surface is covered by salt water, which has the largest water volume, and just about 2.5% of fresh water is available for human consumption. The factors that control the spatio-temporal variability of these water resources are envisaged to be of importance. Hydrometeorology is the branch of science that deals with water resource management and understanding water availability by simultaneously using the principles of hydrology and meteorology. Extreme hydro-meteorological events like floods, droughts, and other hydro-meteorological calamities are impacting the region’s water resources. For a big state such as Madhya Pradesh, where the availability of hydro-meteorological data is critical in dealing with the management of water resources not only for the state but for the other neighbouring states, those aquifers and rivers are fed by the cross-boundary rivers of the state. Several research activities that have been carried out in Madhya Pradesh in hydrometeorology and allied disciplines by various researchers are reviewed and presented in this paper. This research paper also discussed the analysis of hydrometeorology services and highlighted the significance of hydrometeorology research at regional level. Apart from this, the major challenges faced in hydro-meteorological research in Madhya Pradesh are also highlighted in the paper.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 9","pages":"2935 - 2948"},"PeriodicalIF":1.9,"publicationDate":"2024-08-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142209930","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Kum-Ryong Jo, Song-Ryong Kim, Ki-Song Pak, Hyok-Chol Kim, Yong-Sik Ham
{"title":"Impact of Convective and Land Surface Parameterization Schemes on the Simulation of Surface Temperature and Precipitation Using RegCM4.7 During Summer Period Over the DPR Korea","authors":"Kum-Ryong Jo, Song-Ryong Kim, Ki-Song Pak, Hyok-Chol Kim, Yong-Sik Ham","doi":"10.1007/s00024-024-03490-4","DOIUrl":"10.1007/s00024-024-03490-4","url":null,"abstract":"<div><p>This paper has investigated the impact of convective parameterization schemes (CPS) and land surface models (LSM) on the simulation of summer climate over the Democratic People’s Republic of Korea (DPR Korea) using the regional climate model (RegCM 4.7). The sensitivity experiments with two LSMs [Biosphere Atmosphere Transfer Scheme (BATS) and Community Land Model (CLM 3.5)] and four CPSs (Grell, Emanuel, Grell over land and Emanuel over ocean (GL_EO), Emanuel over land and Grell over ocean (EL_GO)) at 30 km horizontal resolution are carried out in summer (from June to August) for 10 years (2001–2010) for this purpose. The simulation results are compared with the available observation data provided from the State Hydro-Meteorological Administration of the DPR Korea (SHMAK). The results show that summer mean circulation patterns (SMCP) and summer averaged surface temperature (SAST) is well captured for most of the simulations, but summer rainfall is not well represented by RegCM 4.7. The performance of the CLM3.5 scheme is better in all the simulations than the BATS scheme. Among the CPSs, the EL_GO scheme shows the smallest biases in the simulation of SAST and summer rainfall. The simulations using EL_GO with CLM3.5 shows the best performance in simulating the SAST and summer rainfall over the study region among the considered CPSs and LSMs. These results will be helpful to improve the prediction of climate change over the DPR Korea.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 8","pages":"2703 - 2715"},"PeriodicalIF":1.9,"publicationDate":"2024-08-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142209929","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
James H. Williams, Ryan Paulik, Rafael Aránguiz, Alec Wild
{"title":"Vulnerability of Physical Infrastructure Network Components to Damage from the 2015 Illapel Tsunami, Coquimbo, Chile","authors":"James H. Williams, Ryan Paulik, Rafael Aránguiz, Alec Wild","doi":"10.1007/s00024-024-03550-9","DOIUrl":"10.1007/s00024-024-03550-9","url":null,"abstract":"<div><p>This study assesses physical infrastructure vulnerability for infrastructure network components exposed during the 2015 Illapel tsunami in Coquimbo, Chile. We analyse road and utility pole vulnerability to damage, based on interpolated and simulated tsunami hazard intensity (flow depth, flow velocity, hydrodynamic force and momentum flux) and network component characteristics. A Random Forest Model and Spearman’s Rank correlation test are applied to analyse variable importance and monotonic relationships, with respect to damage, between tsunami hazards and network component attributes. These models and tests reveal that flow depth correlates higher with damage, relative to flow velocity, hydrodynamic force and momentum flux. Scour (for roads and utility poles) and debris strikes (for utility poles) are strongly correlated with damage. A cumulative link model methodology is used to fit fragility curves. These fragility curves reveal that, in response to flow depth, Coquimbo roads have higher vulnerability than those analysed in previous tsunami event studies, while utility poles demonstrate lower vulnerability than with previous studies. Although we identify tsunami flow depth as the most important hydrodynamic hazard intensity metric, for causing road and utility pole damage, multiple characteristics correlate with damage and should also be considered when classifying infrastructure damage levels.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 8","pages":"2421 - 2445"},"PeriodicalIF":1.9,"publicationDate":"2024-08-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://link.springer.com/content/pdf/10.1007/s00024-024-03550-9.pdf","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141923852","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Evaluation of Multi-Physics Ensemble Prediction of Monsoon Rainfall Over Odisha, the Eastern Coast of India","authors":"Anshul Sisodiya, Sandeep Pattnaik, Adrish Baneerjee","doi":"10.1007/s00024-024-03547-4","DOIUrl":"10.1007/s00024-024-03547-4","url":null,"abstract":"<div><p>Selecting proper parameterization scheme combinations for a particular application is of great interest to Weather Research and Forecasting (WRF) model users. The goal of this research is to create an objective method for identifying a set of scheme combinations to form a Multi-Physics Ensemble (MPE) suitable for short-term precipitation forecasting over Odisha, India’s east coast state. In this study, five member ensembles for Cloud Microphysics (CMP) and Land Surface Model (LSM, conventional ensemble) are created, as well as an ensemble of the top five performing members (optimized ensemble) for 13 Monsoon Depressions (MD) and 8 Deep Depression (DD) cases. There are a total of 30 combinations (5 PBL * 5 CMP, 5 LSM with best PBL and CMP, and one with ISRO Land Use Land Cover data). WRF 4.1 is used to carry out simulations, which are initialized with ERA5 reanalysis data and have a 72-h lead time. Rainfall verification skill scores indicate that ensemble members perform significantly better than any deterministic model. Rainfall characteristics such as location, intensity, and time of occurrence are well predicted in ensemble members as measured by a higher correlation coefficient and a lower RMSE. Neighbourhood ensemble probability also demonstrates that ensemble members have a higher chance of detecting heavy to very heavy rainfall events with more spatial accuracy. The study also concludes that choice of parameterization also affects large-scale dynamical parameters (temperature, humidity, wind, hydrometeors) and thus associated rainfall. Ensemble members exhibited less bias in the composite analysis of large-scale parameters. Furthermore, a composite analysis of moisture budget components revealed that the convergence term is the most important component of moisture accumulation, resulting in rainfall during the monsoon low-pressure system. These findings indicate that the proposed method is an effective method for reducing bias in rainfall forecasts.</p></div>","PeriodicalId":21078,"journal":{"name":"pure and applied geophysics","volume":"181 8","pages":"2589 - 2611"},"PeriodicalIF":1.9,"publicationDate":"2024-08-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"141969837","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}