Quartz types in shale and their effect on geomechanical properties: An example from the lower Cambrian Niutitang Formation in the Cen'gong block, South China | |
Liu, Jingshou; Ding, Wenlong; Wang, Ruyue; Wu, Zhonghu; Gong, Dajian; Wang, Xinghua; Yin, Shuai; Jiao, Baocheng | |
2018 | |
卷号 | 163页码:100-107 |
URL标识 | 查看原文 |
WOS记录号 | WOS:000442067900011 |
内容类型 | 期刊论文 |
URI标识 | http://www.corc.org.cn/handle/1471x/6011175 |
专题 | 贵州大学 |
作者单位 | 1.[1]China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China 2.[2]China Univ Geosci, Key Lab Marine Reservoir Evolut & Hydrocarbon Abu, Minist Educ, Beijing 100083, Peoples R China 3.[3]China Univ Geosci, Beijing Key Lab Unconvent Nat Gas Geol Evaluat &, Beijing 100083, Peoples R China 4.[4]China Univ Geosci, Key Lab Shale Gas Exploitat & Assessment, Minist Land & Resources, Beijing 100083, Peoples R China 5.[5]SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China 6.[6]Guizhou Univ, Civil Engn, Guiyang 550025, Guizhou, Peoples R China 7.[7]Guizhou Univ, Sch Resource & Environm Engn, Guiyang 550025, Guizhou, Peoples R China 8.[8]China Energy Reserve Corp, Beijing 100107, Peoples R China 9.[9]Tongren Sinoenergy Nat Gas Corp, Tongren 554300, Peoples R China 10.[10]Xian Shiyou Univ, Sch Earth Sci & Engn, Xian 710065, Shaanxi, Peoples R China |
推荐引用方式 GB/T 7714 | Liu, Jingshou,Ding, Wenlong,Wang, Ruyue,et al. Quartz types in shale and their effect on geomechanical properties: An example from the lower Cambrian Niutitang Formation in the Cen'gong block, South China[J],2018,163:100-107. |
APA | Liu, Jingshou.,Ding, Wenlong.,Wang, Ruyue.,Wu, Zhonghu.,Gong, Dajian.,...&Jiao, Baocheng.(2018).Quartz types in shale and their effect on geomechanical properties: An example from the lower Cambrian Niutitang Formation in the Cen'gong block, South China.,163,100-107. |
MLA | Liu, Jingshou,et al."Quartz types in shale and their effect on geomechanical properties: An example from the lower Cambrian Niutitang Formation in the Cen'gong block, South China".163(2018):100-107. |
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