Distinctive spatial-temporal evolution of Late Paleozoic to Mesozoic magmatic systems in Northeast Asia: Evidences for identification of the extent and superposition of multiple plate tectonic regimes

doi:10.13745/j.esf.sf.2022.2.5

Abstract

Abstract:

The tectonic evolution of Northeast Asia has experienced the collision and post-collision processes of the Paleo-Asian Ocean, the Mongol-Okhotsk Ocean and the Paleo-Pacific Ocean. However, the spatial-temporal distribution ranges and overlapping processes of these three tectonic regimes have long been difficult to constrain properly. In this paper, we analyzed the spatial-temporal migration patterns of Late Paleozoic-Mesozoic magmatic rocks of Northeast Asia through the constructions of U-Pb age data of giant magmatic belts and a series of data-driven digital maps, with the aim to constrain the tectonic superimposition of the three tectonic regimes. We determined that the extent of each tectonic domain varies in different periods. During the Permian to Jurassic, Paleo-Asian Ocean experienced subduction and collision, which affected mainly the Alxa-northern margin of North China Craton-Da Hinggan Mountains areas; while the Okhotsk Ocean was mainly a continental margin environment, and its influence was initially limited to the central and northern Mongolia and areas around Baikal and then gradually extended to the Mongol-Okhotsk main suture zone in the Jurassic. In the Cretaceous, the Okhotsk Ocean orogenic belt extended and collapsed, which further expanded its influence, with its long-range effect reaching the areas affected by the Paleo-Asian Ocean. Meanwhile, the Paleo-Pacific tectonic system mainly developed in the Triassic to Jurassic, and its plate subduction reached the Da Hinggan-Taihang Mountains area-a gravity gradient zone in the eastern Asian continent, with its long range effect subsequently reaching the easternmost margin of the eastern Asian continent due to the subducting plate retreating during the Cretaceous. Thus, these processes of were superimposed on the products of the Paleo-Asian Oceanic system, together with these of the Mongol-Okhotsk Oceanic system, they all superimposed mainly on the Da Hinggan Mountains region.

Key words: spatial-temporal distribution of magmatism, tectonic superimposition, Mongol-Okhotsk regime, Circum-Pacific regime, Paleo-Asian Ocean regime, magmatic migration, Northeast Asia

CLC Number:

P542
P588.1

WANG Tao, ZHANG Jianjun, LI Shan, TONG Ying, GUO Lei, ZHANG Xiaowei, HUANG He, ZHANG Lei, XUE Huaimin. Distinctive spatial-temporal evolution of Late Paleozoic to Mesozoic magmatic systems in Northeast Asia: Evidences for identification of the extent and superposition of multiple plate tectonic regimes[J]. Earth Science Frontiers, 2022, 29(2): 28-44.

Figures/Tables 8

Fig.1 Tectonic sketch map of Northeast Asia. Modified after 1.

Fig.2 Distribution map of Late Paleozoic-Cenozoic granitoids and related magmatic rocks of Northeast Asia

Fig.3 Histogram of the rock areas of Late Paleozoic-Cenozoic granitoids and related magmatic rocks of Northeast Asia

Fig.4 Distribution of granitoids and related igneous rocks of Northeast Asia and the extent of the PAO and MOO regimes during the Late Paleozoic (Permian).

Fig.5 Distribution of Early Mesozoic (Triassic) igneous rocks of Northeast Asia and the extent of the three tectonic regimes (PAO, MOO, PPO)

Fig.6 Distribution of Jurassic igneous rocks in Northeast Asia and the extent of the MOO and PPO regimes

Fig.7 Distribution of Cretaceous igneous rocks of Northeast Asia and the extent of the MOO and PPO regimes

Fig.8 Generalized map of Northeast Asian, showing the evolution, transformation and superposition of the three tectonic regimes (PAO, MOO, PPO). Modified after [42, 57].

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