古地理学报 ›› 2022, Vol. 24 ›› Issue (5): 908-919. doi: 10.7605/gdlxb.2022.05.065

• 热烈庆贺西北大学建校120周年 • 上一篇    下一篇

年代古地理学: 理论与实践*

王瑜1, 何登发2, 刘松楠1, 周丽云1, 高山林3   

  1. 1 中国地质大学(北京)科学研究院,北京 100083;
    2 中国地质大学(北京)能源学院,北京 100083;
    3 中国石油化工股份有限公司油田事业部,北京 100728
  • 收稿日期:2022-04-28 修回日期:2022-06-24 出版日期:2022-10-01 发布日期:2022-10-10
  • 作者简介:王瑜,男,1966年生,1988年毕业于西北大学地质学系,现为教授,从事构造年代学、陆内构造变形与机理、大地构造等的教学与科研工作。 E-mail: wangy@cugb.edu.cn。
    *庆贺西北大学建校120周年!
  • 基金资助:
    中国石油长庆油田公司科技攻关项目(编号: ZDZX2021-01)及国家自然科学基金重点项目(编号:41430316)的资助

Chrono-palaeogeography: theory and practice

WANG Yu1, HE Dengfa2, LIU Songnan1, ZHOU Liyun1, GAO Shanlin3   

  1. 1 Institute of Earth Sciences,China University of Geosciences(Beijing),Beijing 100083,China;
    2 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083,China;
    3 Petroleum Exploration and Production Branch of SINOPEC,Beijing 100728,China;
  • Received:2022-04-28 Revised:2022-06-24 Online:2022-10-01 Published:2022-10-10
  • About author:WANG Yu, born in 1966,graduated from Northwest University in 1988. He is a professor in China University of Geosciences(Beijing),studying and teaching on tectonochronology,intracontinental tectonics and their mechanism and tectonics. E-mail: wangy@cugb.edu.cn.
  • Supported by:
    Co-funded by the Project of Tackling the Science and Technology Key Problems in PetroChina Changqing Oil and Gas Field Company(No. ZDZX2021-01)and Major Project of National Natural Science Foundation of China(No.41430316)

摘要: 古地理学研究和探讨的是地质历史时期的地表环境,是构造—环境(气候)—物质相互作用的产物。传统的古地理学及相应的构造古地理、生物古地理学等对大地构造演化及古大陆重建、油气勘探等起到了重要的作用。随着地球演化的深入研究,在多层圈的相互作用,特别是古气候、古环境等研究基础上,需要有机地把地表环境和构造环境相结合,并且综合考虑深层及浅层地质过程对古地理格局的形成和演化的制约。在传统的古地理学基础上,提出一个新的学科——年代古地理学,用以研究和探讨地质历史时期的地表过程。该学科是精细的同位素年代格架下的不同动力学—运动学—物质迁移—环境变迁形成古地理的研究,或者物质—力学—环境(气候)相互作用下的古地理格局的研究。旨在研究和探讨地表过程,亦即形成地表环境的过程,强调同一时间的多元性、不同空间的差异性和不同尺度的穿时性。文中以近年来研究的台湾、扬子及华北克拉通等地区的精细时间尺度下的古地理环境为例,进一步剖析年代古地理学对于重新理解和认识古构造格局演化的重要性。

关键词: 同位素年代学, 古地理学, 多圈层相互作用, 构造—, 环境—, 地表过程, 大陆内部

Abstract: The palaeogeography is to study and understand the earth-surface environment in the geological histories,and it is a product of tectonics-environment(climate)-sedimentation interaction and reaction. The traditional palaeogeography and related tectono-palaeogeography,biopalaeogeography and other subjects have given great contributions to the tectonic evolution,continental reconstruction as well oil-gas exploration and development. More and more works start to focus on the interaction of multiple-layers of the earth,especially the paleo-climate,paleo-environment studies,it's necessary to integrate the earth-surface environment and the tectonic background to reveal the influence of the deep and shallow layers geologic processes on the palaeogeographic framework formation and evolution. We propose a new concept and subject—chrono-palaeogeography to explore the earth surface process and evolution in the geological history. This subject is in a precise isotopic chronological framework to study how the different dynamics-kinematic-material transferring-environment changes shaped the palaeogeography,or how the palaeogeographic framework responded to the interactions or couplings of the materials-tectonics stress-environment(climate). Better than other subjects of the palaeogeography,this subject is for studying and understanding the earth-surface process,but not the environmental state,or the active process to form the earth-surface environment. We emphasize the multiple kinetic factors in a same time,the variation in different spaces,and the diachronous at various scales. In addition,we introduce a few case studies of high precise time constrained palaeogeographic work,such as those studies on the Chinese Taiwan,Yangtze and North China cratons,to show how chrono-palaeogeography improve reconstruction of the continent,tectonic evolution,as well oil-gas exploration.

Key words: chronology, palaeogeography, multiple-layers-cycles interaction, tectonics-environment-earth surface process, intracontinent

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