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扬子陆块下古生界页岩发育特征与沉积模式

徐政语,  蒋恕,  熊绍云,  梁兴,  王高成,  郭燕玲,  何勇,  饶大骞

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文章导航 > 沉积学报  > 2015 >  33(1): 21-35
徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
引用本文: 徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
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XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
Citation: XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
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扬子陆块下古生界页岩发育特征与沉积模式

doi: 10.14027/j.cnki.cjxb.2015.01.003
  • 1.

    中国石油勘探开发研究院杭州地质研究院 杭州 310023;

  • 2.

    犹他大学能源与地球科学研究院 盐湖城 UT84108;

  • 3.

    中国石油浙江油田分公司 杭州 310013

基金项目: 国家重大科技专项(编号:2015ZX05068)、中国石油天然气集团公司重大科技项目(编号:2012F-47-02)与中国石油天然气股份公司科技项目(编号:2012B-0504)基金联合资助
详细信息
    作者简介:

    徐政语 男 1964年出生 博士 高级工程师 构造地质学与石油地质学 E-mail:Xuzy_hz@petrochina.com.cn

  • 中图分类号: P512.2;P595

Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block

  • 1.

    Hangzhou Research Institute of Petroleum Geology, PetroChina, Hangzhou 310023;

  • 2.

    Energy & Geoscience Institute (EGI), University of Utah, Salt Lake City, UT 84108;

  • 3.

    Zhejiang Oilfield company, PetroChina, Hangzhou 310013

    摘要
  • 摘要: 为了深入探讨扬子陆块下古生界页岩发育与分布特征、建立沉积模式,系统收集与整理了扬子陆块下寒武统牛蹄塘组与上奥陶统—下志留统五峰—龙马溪组两套富有机质页岩大量数据,选取贵州省三都县渣拉沟及四川省筠连县昭104井两个典型剖面与井岩芯进行了系统观察与采样,对扬子陆块范围内两套富有机质页岩岩性与沉积相发育特征进行了系统分析.研究表明,早古生代以来,扬子陆块受被动大陆边缘扩张与陆缘造山挠曲坳陷两类成盆环境影响[1-2],牛蹄塘组页岩沉积于被动大陆边缘扩张环境,缘于上升洋流与缺氧事件复合沉积模式,富有机质页岩以扬子陆块东南缘深水陆棚—斜坡相区最为发育、厚度最大、有机碳含量最高;五峰—龙马溪组页岩沉积于加里东期周缘前陆造山环境,缘于浅水陆棚—闭塞滞留海湾沉积模式,富有机质页岩以中上扬子陆块东南缘深水陆棚区最为发育、厚度最大、有机碳含量最高.
    Abstract: To further investigate the Paleozoic organic-rich shale development and distribution characteristics in the Yangtze Continental Block, and the depositional model, we systematically collected and compiled large data sets of organic-rich shales for the Lower Cambrian Niutitang equivalent Formation and Upper Ordovician Wufeng-Lower Silurian Longmaxi equivalent Formation. Outcrop in Zhalagou of Sandu county, Guizhou province and Zhao 104 wells Junlian Prefecture, Sichuan Province were selected for the systematic observation, sample tests, sedimentary facies, and so on. Regional reconstruction of paleogeography and correlation between different regions show that the Yangtze block was passive continental margin during the early Paleozoic and peripheral foreland during early Silurian. Niutitang equivalent shales were deposited in a passive continental margin environment, the upwelling nutrient flow and anoxic events in complex depositional model is interpreted for the depositional model of Lower Cambrian shale in Yangtze Block, organic-rich thick shale was mainly developed in the southeastern margin of the Yangtze block deep water shelf to slope facies; Ordovician Wufeng- Lower Silurian Longmaxi equivalent shales were deposited in the Caledonian orogenic front of the periphery foreland environment, organic-rich thick shale was mainly developed in in the anoxic intra-shelf low setting in southeastern margin of the Upper to middle Yangtze block.
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    [79] 李娟,于炳松,郭峰. 黔北地区下寒武统底部黑色页岩沉积环境条件与源区构造背景分析[J]. 沉积学报,2013,31(1): 20-31.[Li Juan, Yu Bingsong, Guo Feng. Depositional setting and tectonic background analysis on Lower Cambrian black shales in the North of Guizhou province[J]. Acta Sedimentologica Sinica, 2013, 31(1): 20-31.]
    [80] 魏怀瑞,杨瑞东,鲍淼,等. 贵州早寒武世黑色页岩地球化学特征及其意义[J]. 贵州大学学报: 自然科学版,2007,23(4): 356-360.[Wei Huairui, Yang Ruidong, Bao Miao, et al. Geochemical characteristics of Early Cambrian black shale in Guizhou province, China [J]. Journal of Guizhou University: Natural Science Edition, 2007, 23(4): 356-360.]
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    [82] 杨恩林,吕新彪,鲍淼,等. 黔东下寒武统黑色页岩微量元素的富集及成因分析[J]. 地球科学进展,2013,28(10): 1160-1169.[Yang Enlin, Lü Xinbiao, Bao Miao, et al. Enrichment and origin of some trace elements in black shales from the Early Cambrian in Eastern Guizhou province[J]. Advances in Earth Science, 2013, 28(10): 1160-1169.]
    [83] 陈旭,张元动,樊隽轩,等. 广西运动的进程: 来自生物相和岩相带的证据[J]. 中国科学(D辑): 地球科学,2012,42(11): 1617-1626.[Chen Xu, Zhang Yuandong, Fan Junxuan, et al. Process of Guangxi movement: Evidence from biological phase and facies belts [J]. Science China(Series D): Earth Sciences, 2012, 42(11): 1617-1626.]
    [84] 刘树根,王世玉,孙玮,等. 四川盆地及其周缘五峰组龙马溪组黑色页岩特征[J]. 成都理工大学学报: 自然科学版,2013,40(6): 621-639.[Liu Shugen, Wang Shiyu, Sun Wei, et al. Characteristics of block shale in Wufeng Formation and Longmaxi Formation in Sichuan Basin and its peripheral areas[J]. Journal of Chengdu University of Technology: Science and Technology Edition, 2013, 40(6): 621-639.]
    [85] 陈旭,戎嘉余. 从生物地层学到大地构造学——以华南奥陶系和志留系为例[J]. 现代地质,1999,13(4): 385-389.[Chen Xu, Rong Jiayu. From biostratigraphy to tectonics—with Ordovician and Silurian of South China as an example[J]. Geoscience, 1999, 13(4): 385-389.]
    [86] 严德天,陈代钊,王清晨,等. 扬子地区奥陶系—志留系界线附近地球化学研究[J]. 中国科学(D辑): 地球科学,2009,39(3): 285-299.[Yan Detian, Chen Daizhao, Wang Qingchen, et al. Geochemical study of Yangtze Ordovician - Silurian boundary near[J]. Science China(Series D): Earth Sciences, 2009, 39(3): 285-299.]
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出版历程
  • 收稿日期:  2014-02-24
  • 修回日期:  2014-04-25
  • 刊出日期:  2015-02-10

目录

    扬子陆块下古生界页岩发育特征与沉积模式

    doi: 10.14027/j.cnki.cjxb.2015.01.003
    • 1. 中国石油勘探开发研究院杭州地质研究院 杭州 310023;
    • 2. 犹他大学能源与地球科学研究院 盐湖城 UT84108;
    • 3. 中国石油浙江油田分公司 杭州 310013
      • 基金项目:  国家重大科技专项(编号:2015ZX05068)、中国石油天然气集团公司重大科技项目(编号:2012F-47-02)与中国石油天然气股份公司科技项目(编号:2012B-0504)基金联合资助
      作者简介:

      徐政语 男 1964年出生 博士 高级工程师 构造地质学与石油地质学 E-mail:Xuzy_hz@petrochina.com.cn

    • 收稿日期: 2014-02-24
    • 修回日期: 2014-04-25
    • 刊出日期: 2015-02-10

    • 中图分类号: P512.2;P595

    摘要: 为了深入探讨扬子陆块下古生界页岩发育与分布特征、建立沉积模式,系统收集与整理了扬子陆块下寒武统牛蹄塘组与上奥陶统—下志留统五峰—龙马溪组两套富有机质页岩大量数据,选取贵州省三都县渣拉沟及四川省筠连县昭104井两个典型剖面与井岩芯进行了系统观察与采样,对扬子陆块范围内两套富有机质页岩岩性与沉积相发育特征进行了系统分析.研究表明,早古生代以来,扬子陆块受被动大陆边缘扩张与陆缘造山挠曲坳陷两类成盆环境影响[1-2],牛蹄塘组页岩沉积于被动大陆边缘扩张环境,缘于上升洋流与缺氧事件复合沉积模式,富有机质页岩以扬子陆块东南缘深水陆棚—斜坡相区最为发育、厚度最大、有机碳含量最高;五峰—龙马溪组页岩沉积于加里东期周缘前陆造山环境,缘于浅水陆棚—闭塞滞留海湾沉积模式,富有机质页岩以中上扬子陆块东南缘深水陆棚区最为发育、厚度最大、有机碳含量最高.

    English Abstract

    徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
    引用本文: 徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
    shu
    XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
    Citation: XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
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