显生宙全球古板块再造及构造演化

doi:10.7623/syxb201402001

石油学报 ›› 2014, Vol. 35 ›› Issue (2): 207-218.DOI: 10.7623/syxb201402001

• 地质勘探 • 下一篇

显生宙全球古板块再造及构造演化

李江海, 王洪浩, 李维波, 周肖贝

北京大学地球与空间科学学院造山带与地壳演化教育部重点实验室北京大学石油与天然气研究中心北京 100871

收稿日期:2013-10-03 修回日期:2014-01-16 出版日期:2014-03-25 发布日期:2014-04-11
通讯作者: 王洪浩，男，1989年10月生，2012年获北京大学地球与空间科学学院理学学士学位，现为北京大学地球与空间科学学院博士研究生，主要从事构造地质学研究。Email：whhpeking@163.com
作者简介:李江海，男，1965年7月生，1986年获北京大学地质系理学学士学位，1992年获北京大学地质系理学博士学位，现为北京大学地球与空间科学学院教授、博士生导师，主要从事大地构造及油气构造研究。Email：jhli@pku.edu.cn
基金资助:
国家重点基础研究发展计划（973）项目（2009CB219302）资助。

Discussion on global tectonics evolution from plate reconstruction in Phanerozoic

Li Jianghai, Wang Honghao, Li Weibo, Zhou Xiaobei

Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Institute of Oil and Gas, Peking University, Beijing 100871, China

Received:2013-10-03 Revised:2014-01-16 Online:2014-03-25 Published:2014-04-11

摘要/Abstract

摘要：

基于前人对全球古板块构造演化的研究成果、最新的古地磁数据库和ArcGIS方法，辅以洋壳扩张、俯冲带以及区域构造等研究成果，完成了对显生宙以来全球古板块的再造及构造演化探讨。相比前人研究，本系列图件采用了最新数据，加强了高质量数据在板块再造中的权重，并通过“幔源法”对部分板块的古经度进行了校正，同时细化了对中国3大陆块的研究。全球显生宙以来的构造演化涉及到潘诺提大陆、冈瓦纳大陆、劳俄大陆、泛大陆的聚合和裂解旋回及多个大洋盆地的扩张和闭合。中生代—新生代以来不同构造域的发育与消亡在时空上具有此消彼长的关系，造成洋陆格局的变迁和大陆面积的持续增加。不同板块的聚合过程常伴随长距离漂移、大幅度旋转运动以及聚合后的减速。新、老超大陆之间以翻夹模式裂解和聚合，即随着超大陆内部裂解、扩张，外侧聚敛、旋转，逐渐发生内、外板块边界的转折。泛大陆构造格局具有动态变化的特征，二叠纪规模最大，其形态不完整，有扇状洋盆缺口（古特提斯洋）持续扩张以及板内走滑运动调整。泛大陆聚合过程中至少出现4种板块汇聚碰撞方式：追尾式碰撞、侧向式碰撞、错车式碰撞和拥堵式碰撞。

关键词: 古板块再造, 显生宙, 泛大陆, 冈瓦纳, 构造演化, 构造域

Abstract:

In this study, we compile Phanerozoic global plate reconstruction maps and discuss relevant tectonic evolution based on previous research findings, the latest paleomagnetic database and ArcGIS method, and research achievements regarding oceanic crustal spreading, subduction belts, and regional tectonics. Compared with the existing global plate reconstruction maps, our constructed maps are superior with the latest paleomagnetic data of high quality and increased weight. Further, we correct the paleo-longtitude of specific plates by using the plume generation zone method and refine the reconstruction of three major blocks of China. Global phanerozoic tectonic evolution involves the convergence and breakup of multiple supercontinents (including Pannotia, Gondwana, Laurussia, and Pangaea) and the spreading and closing of oceanic basins. Since the Mesozoic-Cenozoic period, the development and extinction of tectonic domains had a reciprocal spatiotemporal relationship, leading to the changes in ocean-continent framework and sustainable increases in continental area. The convergence of supercontinents was commonly associated with long-distance drifting, large-scale rotation, and late deceleration. The old and new supercontinents converged and broke up in a flipping model, that is, the inter continent broke up and expanded while the outer one converged and rotated, gradually leading to the transition. The tectonic framework of Pangaea was dynamic, which maximized in the Permian with intact morphology, continuous spreading of fan-shaped gaps, and intraplate adjustment through strike-slip movement. Associated plate collision occurred in at least four patterns, including rear-end collision, lateral collision, rubbing collision, and congestion collision.

Key words: plate reconstruction, Phanerozoic, Pangaea, Gondwana, tectonic evolution, tectonic domain

中图分类号:

TE111.2

李江海, 王洪浩, 李维波, 周肖贝. 显生宙全球古板块再造及构造演化[J]. 石油学报, 2014, 35(2): 207-218.

Li Jianghai, Wang Honghao, Li Weibo, Zhou Xiaobei. Discussion on global tectonics evolution from plate reconstruction in Phanerozoic[J]. ACTA PETROLEI SINICA, 2014, 35(2): 207-218.

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显生宙全球古板块再造及构造演化

Discussion on global tectonics evolution from plate reconstruction in Phanerozoic

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