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三叠纪全球板块再造及岩相古地理研究

塔斯肯 李江海 李维波 王洪浩 杨静懿 李文山

塔斯肯, 李江海, 李维波, 王洪浩, 杨静懿, 李文山. 三叠纪全球板块再造及岩相古地理研究[J]. 海洋地质与第四纪地质, 2014, 34(5): 153-162. doi: 10.3724/SP.J.1140.2014.05153
引用本文: 塔斯肯, 李江海, 李维波, 王洪浩, 杨静懿, 李文山. 三叠纪全球板块再造及岩相古地理研究[J]. 海洋地质与第四纪地质, 2014, 34(5): 153-162. doi: 10.3724/SP.J.1140.2014.05153
Abitkazy Taskyn, LI Jianghai, LI Weibo, YANG Jingyi, WANG Honghao, LI Wenshan. RESEARCH ON GLOBAL PALEO-PLATE RECONSTUCTION AND LITHOFACIES PALAEOGEOGRAPHY IN TRIASSIC[J]. Marine Geology & Quaternary Geology, 2014, 34(5): 153-162. doi: 10.3724/SP.J.1140.2014.05153
Citation: Abitkazy Taskyn, LI Jianghai, LI Weibo, YANG Jingyi, WANG Honghao, LI Wenshan. RESEARCH ON GLOBAL PALEO-PLATE RECONSTUCTION AND LITHOFACIES PALAEOGEOGRAPHY IN TRIASSIC[J]. Marine Geology & Quaternary Geology, 2014, 34(5): 153-162. doi: 10.3724/SP.J.1140.2014.05153

三叠纪全球板块再造及岩相古地理研究


doi: 10.3724/SP.J.1140.2014.05153
详细信息
    作者简介:

    塔斯肯(1985-),男,哈萨克斯坦共和国,北京大学地球与空间科学学院硕士研究生,主要从事含油气盆地与盆地动力学研究,E-mail:taskyn710@gmail.ru

  • 基金项目:

    国家重点基础研究发展规划项目(2009CB219302)

  • 中图分类号: P736.1

RESEARCH ON GLOBAL PALEO-PLATE RECONSTUCTION AND LITHOFACIES PALAEOGEOGRAPHY IN TRIASSIC

More Information
  • 摘要: 三叠纪全球古板块再造及岩相古地理的研究对分析该时期烃源岩全球分布特征及形成环境具有重要意义。利用古地磁软件恢复三叠纪全球古板块再造图,并在此基础上结合全球盆地分析和理论框架,叠加更新各种地质要素,最终编制完成三叠纪全球古地理图、全球岩相及烃源岩分布图。早三叠世发生泛大陆持续汇聚事件,导致在全球范围内火山频繁活动、冰川消融及弧后盆地的广泛发育;由于格陵兰和波罗的之间的多个热点,以及中大西洋大火山岩省的岩浆作用,导致中-晚三叠世泛大陆开始裂解,全球海平面上升,大陆周缘广泛发育陆表海,提供了利于生烃母质生物繁衍生息的环境,继而促进了烃源岩的形成。三叠纪的烃源岩仅占全显生宙时期的1.2%,干酪根类型分布较为均一。
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三叠纪全球板块再造及岩相古地理研究

doi: 10.3724/SP.J.1140.2014.05153
    作者简介:

    塔斯肯(1985-),男,哈萨克斯坦共和国,北京大学地球与空间科学学院硕士研究生,主要从事含油气盆地与盆地动力学研究,E-mail:taskyn710@gmail.ru

基金项目:

国家重点基础研究发展规划项目(2009CB219302)

  • 中图分类号: P736.1

摘要: 三叠纪全球古板块再造及岩相古地理的研究对分析该时期烃源岩全球分布特征及形成环境具有重要意义。利用古地磁软件恢复三叠纪全球古板块再造图,并在此基础上结合全球盆地分析和理论框架,叠加更新各种地质要素,最终编制完成三叠纪全球古地理图、全球岩相及烃源岩分布图。早三叠世发生泛大陆持续汇聚事件,导致在全球范围内火山频繁活动、冰川消融及弧后盆地的广泛发育;由于格陵兰和波罗的之间的多个热点,以及中大西洋大火山岩省的岩浆作用,导致中-晚三叠世泛大陆开始裂解,全球海平面上升,大陆周缘广泛发育陆表海,提供了利于生烃母质生物繁衍生息的环境,继而促进了烃源岩的形成。三叠纪的烃源岩仅占全显生宙时期的1.2%,干酪根类型分布较为均一。

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