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黔北地区下寒武统牛蹄塘组泥岩沉积环境及页岩气勘探潜力
何洪茜; 肖加飞; 杨海英; 兰青; 黄明亮
2024
Source Publication沉积与特提斯地质
Volume44Issue:2Pages:267-277
Abstract
寒武系下统牛蹄塘组是中国南方海相碳质页岩赋存的主要层位之一,在贵州北部、中部及东部广泛分布,层位稳定。牛蹄塘组以黑色炭质泥岩为主,岩层多为薄层状,具水平层理,其组分主要为黏土矿物、石英及少量的碳质组分和黄铁矿。与澳大利亚后太古代页岩(PAAS)平均值相比,泥岩V、Mo、U含量较高,而Co、Cu、Zn和Th含量较低。V/Cr、Ni/Co、U/Th、V/(V+Ni)的元素比值以及AU含量表明,牛蹄塘组黑色泥岩沉积环境呈缺氧还原状态。样品(La/Yb)N值明显大于1,轻、重稀土元素分异程度较大,指示沉积速率较低。有机质丰度较高,有机质成熟度为高—过成熟阶段,脆性矿物含量较高,有效厚度约为30~100 m。综上,黔北牛蹄塘组黑色泥岩存在形成页岩气藏的较好物质条件,具有良好的页岩气勘探潜力。
 
Keyword牛蹄塘组 页岩气 沉积环境 勘探潜力 黔北
DOI10.19826/j.cnki.1009-3850.2023.03002
Indexed ByCSCD
Language中文
CSCD IDCSCD:7759882
Citation statistics
Cited Times:2[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/15576
Collection矿床地球化学国家重点实验室
Affiliation1.中国科学院地球化学研究所矿床地球化学国家重点实验室
2.中国科学院大学
Recommended Citation
GB/T 7714
何洪茜,肖加飞,杨海英,等. 黔北地区下寒武统牛蹄塘组泥岩沉积环境及页岩气勘探潜力[J]. 沉积与特提斯地质,2024,44(2):267-277.
APA 何洪茜,肖加飞,杨海英,兰青,&黄明亮.(2024).黔北地区下寒武统牛蹄塘组泥岩沉积环境及页岩气勘探潜力.沉积与特提斯地质,44(2),267-277.
MLA 何洪茜,et al."黔北地区下寒武统牛蹄塘组泥岩沉积环境及页岩气勘探潜力".沉积与特提斯地质 44.2(2024):267-277.
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