Late Paleozoic–Mesozoic tectonic evolution of the northeastern Asian continental margin revealed by sedimentary formations and fossil accretionary complexes
Late Paleozoic–Mesozoic tectonic evolution of the northeastern Asian continental margin revealed by sedimentary formations and fossil accretionary complexes
复制标题
沉积地层和化石增生杂岩揭示的东北亚大陆边缘晚古生代—中生代构造演化
DOI：
10.1016/j.earscirev.2021.103908
复制
发表时间：
2021-12
影响因子：
12.1
通讯作者：
Xing-Zhou Zhang
中科院分区：
文献类型：
--
作者：
Yi-Ni Wang;Wen-Liang Xu;Feng Wang;Xing-Zhou Zhang
东北亚大陆边缘晚古生代-中生代构造演化一直是一个有争议的问题。增生杂岩和沉积建造分别作为板块俯冲历史重建和地表响应的直接物质记录，是研究东北亚大陆边缘构造演化的理想标志。本文综述了近年来地质和地球物理研究中有关跃进山、绕河等古火山岩和古火山岩下地壳结构的研究进展，并对这些化石火山岩的岩性、变质变形程度、深部地壳结构和形成时间进行了详细剖析。这些结果与同时代的沉积建造和火成岩组合一起，为东北亚大陆边缘晚古生代-中生代的构造演化提供了新的认识，晚古生代-中生代，东北亚大陆边缘经历了两个构造体制的演化：1）古亚洲洋构造体制阶段，包括晚古生代早期的被动大陆边缘、早二叠世的活动大陆边缘和三叠纪的构造转换。晚泥盆世-晚二叠世，佳木斯地块与一无名地块之间形成古海洋; 2）古太平洋构造体制阶段，包括早侏罗世古太平洋板块俯冲至欧亚大陆之下，晚侏罗世-早白垩世早期侏罗纪AC的增生侵位，晚中生代继续向西俯冲。跃进山AC是古亚洲洋构造体制的产物，形成于晚泥盆世-早二叠世。最后一次侵位发生在二叠纪晚期。饶河AC是古太平洋构造体制的产物，经历了中-晚侏罗世海山形成和陆源碎屑沉积、晚侏罗世海山-欧亚大陆碰撞、晚侏罗世-早白垩世早期饶河AC胚胎北移等阶段早白垩世晚期（140 - 130 Ma），饶河AC最终侵位。
The Late Paleozoic–Mesozoic tectonic evolution in the northeastern (NE) Asian continental margin has been a controversial issue. Accretionary complexes (ACs) and sedimentary formations, as the direct material records of the reconstruction of plate subduction history and surface response, respectively, are the categorically ideal indicators to explore tectonic evolution of the NE Asian continental margin. This study reviews recent geological and geophysical advances about the crustal structures beneath the massifs and ACs such as the Yuejinshan and Raohe ACs and conducts a detailed dissection on lithology, degree of metamorphism and deformation, deep crustal structure, and formation time of these fossil ACs. These results, together with the coeval sedimentary formations and igneous rock associations, provide new insights for Late Paleozoic-Mesozoic tectonic evolution of NE Asian continental margin, i.e., the NE Asian continental margin experienced the evolution of two tectonic regimes during the Late Paleozoic–Mesozoic: 1) the stage of the Paleo-Asian Ocean tectonic regime, including a passive continental margin in the early stage of the Late Paleozoic, an active continental margin in the early Permian, and tectonic transition in the Triassic. A paleo-ocean occurred between the Jiamusi Massif and an unnamed massif during the Late Devonian–late Permian; and 2) the stage of the Paleo-Pacific tectonic regime, including the subduction onset of the Paleo-Pacific Plate beneath Eurasia in the Early Jurassic, the accretion and emplacement of the Jurassic ACs during the Late Jurassic–early Early Cretaceous, and the continuous westward subduction during the Late Mesozoic. The Yuejinshan AC was the product of the Paleo-Asian Ocean tectonic regime and formed during the Late Devonian–early Permian. Its final emplacement occurred in the late Permian. The Raohe AC was the product of the Paleo-Pacific tectonic regime and experienced the following stages: 1) the formation of seamounts and deposition of the terrigenous clastic sediments in the Middle–Late Jurassic; 2) the seamount–Eurasia collision in the Late Jurassic; 3) the northward migration of the embryo of the Raohe AC during the Late Jurassic–early Early Cretaceous (160–140 Ma); 4) the deposition of the early Early Cretaceous sediments; and 5) the final emplacement of the Raohe AC in the late Early Cretaceous (140–130 Ma).
登录
查看更多内容
黑龙江省东部晚古生代沉积岩碎屑-锆石年代学：对中亚造山带东段构造演化的启示
影响因子：
2.9
作者：
Xu, Wen-Liang;Yu, Yang;Zhang, Xing-Zhou;Pei, Fu-Ping;Yang, De-Bin;Meng, En
通讯作者：
Meng, En
中国东北敦化-密山断裂带中生代走滑运动对大洋板块俯冲的响应
影响因子：
2.9
作者：
Cheng Liu;Guang Zhu;Shuai Zhang;Chengchuan Gu;Yunjian Li;Nan Su;Shiye Xiao
通讯作者：
Shiye Xiao
影响因子：
4.2
作者：
Jian‐Bo Zhou;Jia-Lin Cao;S. Wilde;Guochun Zhao;Jinjiang Zhang;Bin Wang
通讯作者：
Jian‐Bo Zhou;Jia-Lin Cao;S. Wilde;Guochun Zhao;Jinjiang Zhang;Bin Wang
影响因子：
1.8
作者：
Cheng Rui
通讯作者：
Cheng Rui
影响因子：
12.1
作者：
Jian‐Bo Zhou;S. Wilde;Guochun Zhao;Jie Han
通讯作者：
Jian‐Bo Zhou;S. Wilde;Guochun Zhao;Jie Han