Zhaofei Liu , Zhi Chen , Ying Li , Zhidan Zhao , Shunying Hong , Le Hu , Ling Ma , Chang Lu , Yuanxin Zhao , Hongyi He , Shujuan Su , Ying Zhao , Weiye Shao , Zhengyang Cao , Hanyu Wang
{"title":"页岩气泄漏与断层激活:2021 年中国泸县 MS 6.0 级地震的启示","authors":"Zhaofei Liu , Zhi Chen , Ying Li , Zhidan Zhao , Shunying Hong , Le Hu , Ling Ma , Chang Lu , Yuanxin Zhao , Hongyi He , Shujuan Su , Ying Zhao , Weiye Shao , Zhengyang Cao , Hanyu Wang","doi":"10.1016/j.tecto.2024.230530","DOIUrl":null,"url":null,"abstract":"<div><div>In the region of large gas fields, extensive research has been conducted on earthquakes induced by industrial production in shale gas fields. However, limited attention has been given to the impact of post-earthquake events on shale gas reservoir leakage and fault activation. The Luxian <em>M</em><sub>S</sub> 6.0 earthquake, which occurred on 16 September 2021 in the Luzhou shale gas field, has raised concerns about post-earthquake shale gas leakage. Post-earthquake measurements of soil gases (Rn, CO<sub>2</sub>, CH<sub>4</sub>, and H<sub>2</sub>) and isotopic analyses (δ<sup>13</sup>C<sub>CO2</sub>, δ<sup>13</sup>C<sub>CH4</sub> and δD<sub>CH4</sub>) in the Luzhou shale gas field area reveal that the Huayingshan fault zone, a natural pathway for shale gas leakage, was not activated by the Luxian earthquake and did not exhibit any further shale gas leakage after the 2021 earthquake. Furthermore, the seismogenic fault, which was impacted by the earthquake, did not damage the shale gas reservoir, causing shale gas leakage. This study provides an important foundation for future research on shale gas extraction and seismic activity in the region.</div></div>","PeriodicalId":22257,"journal":{"name":"Tectonophysics","volume":"891 ","pages":"Article 230530"},"PeriodicalIF":2.7000,"publicationDate":"2024-10-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Shale gas leakage and fault activation: Insight from the 2021 Luxian MS 6.0 earthquake, China\",\"authors\":\"Zhaofei Liu , Zhi Chen , Ying Li , Zhidan Zhao , Shunying Hong , Le Hu , Ling Ma , Chang Lu , Yuanxin Zhao , Hongyi He , Shujuan Su , Ying Zhao , Weiye Shao , Zhengyang Cao , Hanyu Wang\",\"doi\":\"10.1016/j.tecto.2024.230530\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>In the region of large gas fields, extensive research has been conducted on earthquakes induced by industrial production in shale gas fields. However, limited attention has been given to the impact of post-earthquake events on shale gas reservoir leakage and fault activation. The Luxian <em>M</em><sub>S</sub> 6.0 earthquake, which occurred on 16 September 2021 in the Luzhou shale gas field, has raised concerns about post-earthquake shale gas leakage. Post-earthquake measurements of soil gases (Rn, CO<sub>2</sub>, CH<sub>4</sub>, and H<sub>2</sub>) and isotopic analyses (δ<sup>13</sup>C<sub>CO2</sub>, δ<sup>13</sup>C<sub>CH4</sub> and δD<sub>CH4</sub>) in the Luzhou shale gas field area reveal that the Huayingshan fault zone, a natural pathway for shale gas leakage, was not activated by the Luxian earthquake and did not exhibit any further shale gas leakage after the 2021 earthquake. Furthermore, the seismogenic fault, which was impacted by the earthquake, did not damage the shale gas reservoir, causing shale gas leakage. This study provides an important foundation for future research on shale gas extraction and seismic activity in the region.</div></div>\",\"PeriodicalId\":22257,\"journal\":{\"name\":\"Tectonophysics\",\"volume\":\"891 \",\"pages\":\"Article 230530\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2024-10-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Tectonophysics\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0040195124003329\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Tectonophysics","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0040195124003329","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Shale gas leakage and fault activation: Insight from the 2021 Luxian MS 6.0 earthquake, China
In the region of large gas fields, extensive research has been conducted on earthquakes induced by industrial production in shale gas fields. However, limited attention has been given to the impact of post-earthquake events on shale gas reservoir leakage and fault activation. The Luxian MS 6.0 earthquake, which occurred on 16 September 2021 in the Luzhou shale gas field, has raised concerns about post-earthquake shale gas leakage. Post-earthquake measurements of soil gases (Rn, CO2, CH4, and H2) and isotopic analyses (δ13CCO2, δ13CCH4 and δDCH4) in the Luzhou shale gas field area reveal that the Huayingshan fault zone, a natural pathway for shale gas leakage, was not activated by the Luxian earthquake and did not exhibit any further shale gas leakage after the 2021 earthquake. Furthermore, the seismogenic fault, which was impacted by the earthquake, did not damage the shale gas reservoir, causing shale gas leakage. This study provides an important foundation for future research on shale gas extraction and seismic activity in the region.
期刊介绍:
The prime focus of Tectonophysics will be high-impact original research and reviews in the fields of kinematics, structure, composition, and dynamics of the solid arth at all scales. Tectonophysics particularly encourages submission of papers based on the integration of a multitude of geophysical, geological, geochemical, geodynamic, and geotectonic methods