Mesozoic superposed orogenic system in eastern China

doi:10.13745/j.esf.sf.2023.7.15

Abstract

Abstract:

The Indosinian and Yanshanian orogenic movements are both important Mesozoic orogenies in eastern China. The resulted tectonic belts are neither products of the third stage of crustal evolution, as proposed by Chen Guoda, nor intracontinental (or intraplate) orogenic belts generated by intraplate dynamics, as argued by some scholars—rather, they are superposed orogenic belts created on the preformed continental crust in eastern China due to Mosozoic Paleo-Pacific dynamic system. In the past, these orogenic belts were called the peri-Pacific continent-marginal reactivated belts of eastern China. In the Mesozoic, under the effect of Paleo-Pacific dynamic system, the East Asia margin orogenic system formed along Northeast Russia-Sikhote Alin (Russia)-Japan-Ryukyu-Taiwan (China)-Palawan (Philippines) regions, while simultaneously the Mesozoic superposed orogenic system formed in the pre-existing continental crust in eastern China adjacent to the East Asia continental margin. The two orogenic systems, both driven by Mesozoic Paleo-Pacific dynamic system, developed synchronously to form the giant Mesozoic orogenic system in the Pacific tectonic domain in eastern Asia, radically changing the pre-Indosian tectonic framework of eastern Asia.

Key words: superposed orogenic belt, Indosinian orogenic cycle, Yanshanian orogenic cycle, Mesozoic superposed orogenic system of eastern China, Pacific tectonic domain

CLC Number:

P544
P542

REN Jishun, LIU Jianhui, ZHU Junbin. Mesozoic superposed orogenic system in eastern China[J]. Earth Science Frontiers, 2024, 31(1): 142-153.

Figures/Tables 7

References 58

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造山旋回	期次	地层
燕山造山旋回	第3幕	上覆代表性地层:Albian期登娄库组/东井组上限年龄:(110±5) Ma 造山运动时代:早白垩世晚期
	第2幕	上覆代表性地层:Valanginian-Hauterivian张家口火山岩上限年龄:135 Ma 造山运动时代:晚侏罗世中晚期—白垩纪初
	第1幕	上覆代表性地层:Bajocian-Bothonian髫髻山组/蓝旗组上限年龄:(165±5) Ma 造山运动时代:中侏罗世中期
印支造山旋回	第3幕	上覆代表性地层:早侏罗世晚期—中侏罗世初象山组/北票组上限年龄:(190±5) Ma 造山运动时代:晚三叠世末—侏罗纪初
	第2幕	上覆代表性地层:Norian安源煤系/艮口组上限年龄:220 Ma 造山运动时代:中三叠世末—晚三叠世早期
	第1幕	上覆代表性地层:早三叠世地层上限年龄:250 Ma 造山运动时代:晚二叠世晚期

造山旋回	期次	地层
燕山造山旋回	第3幕	上覆代表性地层:Albian期登娄库组/东井组上限年龄:(110±5) Ma 造山运动时代:早白垩世晚期
	第2幕	上覆代表性地层:Valanginian-Hauterivian张家口火山岩上限年龄:135 Ma 造山运动时代:晚侏罗世中晚期—白垩纪初
	第1幕	上覆代表性地层:Bajocian-Bothonian髫髻山组/蓝旗组上限年龄:(165±5) Ma 造山运动时代:中侏罗世中期
印支造山旋回	第3幕	上覆代表性地层:早侏罗世晚期—中侏罗世初象山组/北票组上限年龄:(190±5) Ma 造山运动时代:晚三叠世末—侏罗纪初
	第2幕	上覆代表性地层:Norian安源煤系/艮口组上限年龄:220 Ma 造山运动时代:中三叠世末—晚三叠世早期
	第1幕	上覆代表性地层:早三叠世地层上限年龄:250 Ma 造山运动时代:晚二叠世晚期