华北地台中元古代串岭沟组页岩中的砂脉构造: 17亿年前甲烷气逃逸的沉积标识?

史晓颖; 蒋干清; 张传恒; 刘娟; 高林志

Volume 33 Issue 5

Sep. 2008

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Article Navigation > Earth Science > 2008 > 33(5): 577-590

SHI Xiao-ying, JIANG Gan-qing, ZHANG Chuan-heng, LIU Juan, GAO Lin-zhi, 2008. Sand Veins and Microbially Induced Sedimentary Structures from the Black Shale of the Mesoproterozoic Chuanlinggou Formation (ca. 1.7 Ga) in North China: Implications for Methane Degassing from Microbial Mats. Earth Science, 33(5): 577-590.

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Sand Veins and Microbially Induced Sedimentary Structures from the Black Shale of the Mesoproterozoic Chuanlinggou Formation (ca. 1.7 Ga) in North China: Implications for Methane Degassing from Microbial Mats

1.
School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
State Laboratory of Geological Processes and Mineral Resources, Beijing 100083, China
3.
Department of Geosciences, University of Nevada, Las Vegas, NV 89154-4010, USA
4.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2008-02-27
Publish Date: 2008-09-25

Abstract

Abstract

The Mesoproterozoic Chuanlinggou Formation (ca. 1.7Ga) consists of up to 900m thick, dark-gray to black shale and fine-grained sandstone that are widespread in the North China platform. Abundant centimeter-scale sand veins are present within the black shale layers of this unit, particularly in the central part. Sand veins display ptygmatic shapes, perpendicular or with a high angle to sedimentary bedding. They penetrate the black shale layers but are vertically discontinuous and often terminated by thin, lenticular sandstone beds, forming small-scale 'tepee-like' structures. On bedding planes, sand veins are expressed as small sand ridges with 1-3mm positive relief. Lack of polygonal shapes and their occurrence in thinly laminated, deep-water shale prevent an origin from sand-filled desiccation cracks. Instead, their close association with microbially induced sedimentary structures (MISS), such as micro-wrinkles and gas blisters, and putative bacteria fossils (possibly coccoidal cyanobacteria) and framboidal pyrites, suggests that they were formed by degassing of methane from microbial mat decay. Methane gas disrupted overlying sedimentary layers, creating fractures open to seawater. Fine-grained quartz sands, which were transported into the depositional environment by storm events, filled the open fractures. Sand-filled fractures were shortened and deformed during burial compaction, forming ptygmatic shapes. The presence of dispersed dolomite and siderite in these sand veins suggests authigenic carbonate precipitation from anaerobic oxidation of methane (AOM). Sand veins are mainly distributed within the Chuanlinggou Formation and are spatially widespread in the North China platform. If their methane origin is confirmed, they may have important implications for the Mesoproterozoic plaeoclimate. With a low seawater sulfate concentration during the Mesoproterozoic, methane release from microbial mat decay and/or microbial methanogenesis during shallow burial may have been proportionally higher than that of the modern marine environments, with resultant increase in the relative importance of methane in maintaining the Mesoproterozoic greenhouse climate.
- sand veins,
- methane degassing,
- microbial mats,
- Chuanlinggou Formation,
- Mesoproterozoic,
- North China platform

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References(110)

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Sand Veins and Microbially Induced Sedimentary Structures from the Black Shale of the Mesoproterozoic Chuanlinggou Formation (ca. 1.7 Ga) in North China: Implications for Methane Degassing from Microbial Mats

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