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	Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment - An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin
	Zhu, Dongya; Zhang, Dianwei; Liu, Quanyou; Xing, Fengcun; He, Zhiliang; Zhang, Rongqiang; Liu, Zihao
	2018
卷号	36页码:620-644
URL标识	查看原文
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/3410152
专题	成都理工大学
作者单位	1.[1]SINOPEC, State Key Lab Shale Oil & Gas Enrichment Mech & E, 31 Xueyuan Rd, Beijing 100083, Peoples R China 2.[2]SINOPEC, Lab Struct & Sedimentol Reservoir Geol, Petr Explorat & Prod Res Inst, Beijing, Peoples R China 3.[3]Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu, Sichuan, Peoples R China 4.[4]China Univ Petr, Coll Geosci, Beijing, Peoples R China
推荐引用方式 GB/T 7714	Zhu, Dongya,Zhang, Dianwei,Liu, Quanyou,et al. Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment - An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin[J],2018,36:620-644.
APA	Zhu, Dongya.,Zhang, Dianwei.,Liu, Quanyou.,Xing, Fengcun.,He, Zhiliang.,...&Liu, Zihao.(2018).Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment - An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin.,36,620-644.
MLA	Zhu, Dongya,et al."Formation mechanism of dolomite reservoir controlled by fourth-order sequence in an evaporated marine environment - An example from the Lower Ordovician Tongzi Formation in the Sichuan Basin".36(2018):620-644.

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