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首页|期刊导航|地质学报|黔桂地区泥盆纪富有机质竹节石页岩:一个重要的潜在性页岩气勘探目的层

黔桂地区泥盆纪富有机质竹节石页岩:一个重要的潜在性页岩气勘探目的层

梅冥相 岑文攀 Muhammad RIAZ

地质学报2025,Vol.99Issue(4):1332-1352,21.
地质学报2025,Vol.99Issue(4):1332-1352,21.DOI:10.19762/j.cnki.dizhixuebao.2023081

黔桂地区泥盆纪富有机质竹节石页岩:一个重要的潜在性页岩气勘探目的层

Organic-matter-rich tentaculitid shales of the Devonian in the region from the southern Guizhou to central Guangxi of South China:An importantly potential target rock for shale-gas exploration

梅冥相 1岑文攀 2Muhammad RIAZ3

作者信息

  • 1. 中国地质大学地球科学与资源学院,北京,100083,中国||中国地质大学(北京)生物地质与环境地质国家重点实验室,北京,100083,中国
  • 2. 广西地质调查院,广西南宁,530023,中国
  • 3. 地质研究所,旁遮普大学,拉舍尔,54590,巴基斯坦
  • 折叠

摘要

Abstract

The Devonian period is a significant geological time marked by widespread deposition of organic-matter-rich shales.Within an inter-platform basin facies dominated by deep-water deposits in the region from southern Guizhou to central Guxngxi,a remarkable accumulation of organic-matter-rich tentaculitid shales exceeding 600 meters in thickness developed during the Emsian to Frasnian ages.These shales exhibit characteristics that make them a potential target for shale-gas exploration:① Relatively higher total organic carbon(TOC)values consistently exceed 2%~4%,reaching up to 5%to 6%.② During the early to middle Devonian(Amsian Age),organic carbon content is typically enriched in massive organic-matter-rich tentaculitid shales with the monolayer thickness exceeding 100 meters,formed during periods of third-order relative sea-level rise.Conversely,calcareous shales and muddy limestones of the shelf facies,formed during sea-level falls,exhibit depleted organic carbon content.③ Within the Frasnian Age Liujiang Formation,dominated by silicalites,organic carbon content is typically enriched in massive organic-matter-rich tentaculitid sales with the monolayer ranging from 30 to 40 m thick,formed during the periods of third-order sea-level fall.This contrasts with silicalites of the pelagic basin facies,which show lower organic carbon content during periods of third-order relative sea-level rise.The accumulation of organic matter in these tentaculitid shales is controlled by complicated,nonlinear interactions between productivity,preservation,and sedimentation rates.Importantly,the high density of tentaculitid fossils demonstrates that the accumulation of organic matter within organic-matter-rich tentaculitid shales is genetically related to the biological carbon pump of zooplankton.

关键词

富有机质竹节石页岩/重要的潜在性页岩气勘探目的层/泥盆系/黔桂地区

Key words

organic-matter-rich tentaculitid shale/importantly potential target rock for shale-gas exploration/Devonian/the region from the southern Guizhou to the central Guangxi

引用本文复制引用

梅冥相,岑文攀,Muhammad RIAZ..黔桂地区泥盆纪富有机质竹节石页岩:一个重要的潜在性页岩气勘探目的层[J].地质学报,2025,99(4):1332-1352,21.

基金项目

本文为广西重点研发计划项目(编号2021AB30011)和广西地矿局重点科研项目(编号GXDK202430)资助的成果. (编号2021AB30011)

地质学报

OA北大核心

0001-5717

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