|Table of Contents|

Mechanism, Geological Record and Significance of Subduction Initiation(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2023年第02期
Page:
194-207
Research Field:
基础地质与矿床地质
Publishing date:

Info

Title:
Mechanism, Geological Record and Significance of Subduction Initiation
Author(s):
YANG Gao-xue
(School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China)
Keywords:
plate tectonic subduction initiation ophiolite metamorphic sole forearc basalt boninite mantle plume geological record
PACS:
P541; P691
DOI:
10.19814/j.jese.2022.09011
Abstract:
Initiation of new subduction zones is a fundamental process of Earth's plate tectonics, and it is the key and new direction for the development of plate tectonics theory. Although the subduction initiation has been a focus of research of many scientists during the last 50 years, triggers and mechanisms of subduction initiation remain controversial. Two end-member subduction initiation models have been proposed: spontaneous and induced. Spontaneous subduction initiation mainly includes three models, which are transform collapse, passive margin collapse and plume head margin collapse. Moreover, induced subduction initiation mainly includes subduction transference and polarity reversal. Natural examples of spontaneous and induced subduction initiation have representative geological records of supra-subduction zones(SSZ)ophiolites(ophiolitic mélanges), forearc basalts, boninites and metamorphic soles. These are rock records of upper plate extension and lower plate burial. This will open the door for geologists to contribute fundamentally for understanding subduction initiation. Therefore, a detailed study on geological records of subduction initiation is the basis for unraveling the subduction initiation mechanism, and it is also the most direct and effective means to test the mechanism. In addition, the study of the geological records of subduction initiation can provide constraints on the properties of the mantle, reveal the contribution of different sources to the continental crust accretion, and effectively recover the evolutionary history of the ancient oceanic and related tectonic units, thus providing constraints on their dynamical processes. Although geological records are the key to solve the problem of subduction initiation, these geological records are fragmented and non-systematic in character. In future studies, the geological records should be compared on a large scale so as to form systematic constraints for subduction initiation. Moreover, it should be noted that the existed geological records and subduction initiation may not correspond one by one, i.e., where there is no geological record do not mean there is no subduction initiation. However, in any case, through studying on subduction initiation, it will help for deeply understanding the geometry, kinematics and dynamics of specific plate, and predict plate behavior. Moreover, comparing the evolution of Earth-like planets(such as Mars)will help to unravel the mystery of the uniqueness and habitability of Earth.

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Last Update: 2023-05-20