太平洋古陆的破碎消亡与中新生代华北克拉通板内构造岩浆活化

周瑶琪; 赵士宝

Volume 29 Issue 5

Sep. 2004

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ZHOU Yao-qi, ZHAO Shi-bao, 2004. Disappearing Mystery of Ancient Pacific Land and Its Relationship with Mesozoic-Cenozoic Intraplate Magmatism in North China Craton. Earth Science, 29(5): 575-582.

Citation:

ZHOU Yao-qi, ZHAO Shi-bao, 2004. Disappearing Mystery of Ancient Pacific Land and Its Relationship with Mesozoic-Cenozoic Intraplate Magmatism in North China Craton. Earth Science, 29(5): 575-582.

ZHOU Yao-qi, ZHAO Shi-bao, 2004. Disappearing Mystery of Ancient Pacific Land and Its Relationship with Mesozoic-Cenozoic Intraplate Magmatism in North China Craton. Earth Science, 29(5): 575-582.

Citation:

ZHOU Yao-qi, ZHAO Shi-bao, 2004. Disappearing Mystery of Ancient Pacific Land and Its Relationship with Mesozoic-Cenozoic Intraplate Magmatism in North China Craton. Earth Science, 29(5): 575-582.

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Disappearing Mystery of Ancient Pacific Land and Its Relationship with Mesozoic-Cenozoic Intraplate Magmatism in North China Craton

ZHOU Yao-qi^1
,,
ZHAO Shi-bao²

1.
Geochemistry and Lithosphere Dynamics Laboratory, University of Petroleum, Dongying 257061, China
2.
Fourth Institute of Geological and Mineral Exploration of Inner Mongolia, Jining 012000, China

Received Date: 2004-06-10
Publish Date: 2004-09-25

Abstract

Abstract

This paper reviews the main progress on the impact hypothesis of the Pacific Ocean for the past two decades and discusses the internal and external dynamics mechanism causing disappearance of ancient land of the Pacific Ocean. The impaction event which happened between Permian and Triassic at the Pacific Ocean area resulted in the crash of the Pacific lithospheric plate, and changeed greatly the mode of mantle convection. Under the action driven by the new mantle convection, ancient plate fragments of the Pacific Ocean withered away gradually and coalesced into the adjacent plates around the Pacific Ocean with the collision and subduction of paleo-pacific plate. At the same time, a tectonic system of the surrounding Pacific Ocean began to form. The deep tectonic-thermal regime embracing the surrounding Pacific Ocean tectonic system severely affected the magma activity in the continental plates ajacent Pacific Ocean during Mesozoic and Cenozoic.
- ancient Pacific land,
- impact event,
- mantle convection,
- surrounding Pacific Ocean tectonic system

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References(49)

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