地体的单向和多向聚合与离散
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本文为国家重点研发计划项目(编号2017YFC0601402)资助的研究成果


Unidirectional and multidirectional amalgamation-dispersion of terrane
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    摘要:

    地体构造是对板块构造理论的发展和补充,它受控于全球板块动力学体系,因此不能将地体与板块割裂开来去研究。其相对于刚性板块的小规模、多样性和广泛性,对了解全球板块的离散和大陆的拼贴增生过程具有十分重要意义。地体构造无处不在,它不仅存在于中、新生代陆缘造山带中,也存在于古老造山带中,一些古老的克拉通实际上也是由不同的地体拼合而成的。地体的运动包括聚合、离散和走滑三种方式,地体的增生作用是聚合的主要表现形式,并导致大陆的生长扩大,而地体的离散作用联合增生作用,决定了现代大陆的轮廓。分析地体聚合和离散的过程,可以发现有两种不同的模式,即单向聚合-离散和多向聚合-离散,它们对应了不同的地球动力学过程。地体的单向聚合- 离散可以由大洋的俯冲增生或大陆汇聚碰撞而导致,但在这个过程中,大洋向大陆的单向俯冲起到了主导作用。地体的多向离散和聚合与岩石圈的裂解与汇聚有密切联系,从全球构造演化的格局来看,岩石圈裂解与汇聚的方向本身具有多向性,这就导致了一些微陆块地体与具洋壳性质的地体一同发生多向离散和聚合。地体的单向离散和聚合会因构造变动而转变为多向离散和聚合,俯冲板片回转与海沟后撤会导致俯冲带弯曲和俯冲方向的改变,这是引起上述转变的原因。

    Abstract:

    Terrane tectonics is a supplement to the theory of plate tectonics.As it is controlled by the global plate dynamic system,it cannot be studied separately from the plates.The small size,diversity and pervasiveness of terranes relative to the rigid plates are of great significance in understanding of the divergent process of global plates,and the collage and accretion of continents.Terranesare ubiquitous.They exist not only in Mesozoic and Cenozoic marginal orogenic belts,but also in ancient orogenic belts.Some ancient cratons are actually formed from different terranes.The movement of terranes includes amalgamation,dispersion and strike-slip. The accretion of terranes is the main manifestation of the amalgamation and leads to the growth and expansion of the continent,while the dispersion of terranes combined with the accretion determines the contour of the modern continent.By analyzing the processes of amalgamation and dispersion of terranes,it was determined that there are two different models,namely, unidirectional amalgamation-dispersion and multidirectional amalgamation-dispersion,which correspond to different geodynamic processes.The unidirectional amalgamation-dispersion of terranes can be caused by oceanic subduction-accretion or continental collision,but in this process,the unidirectional subduction of ocean towards continent plays a leading role.The multidirectional amalgamation-dispersion of terranes is closely related to the lithosphere rifting and convergence.From the perspective of the global tectonic evolution pattern,the direction of lithosphere rifting and convergence itself is multidirectional,which leads to the multidirectional dispersion and aggregation of some micro-continents and terranes originated from oceanic crust.The unidirectional dispersion-amalgamation of terrane will change into multidirectional dispersion-amalgamation due to tectonic changes.The roll-back of the subducting slab and the trench retreat will lead to the bending of the subduction zone and the change of the subduction direction,which are the reasons for the above transformation.

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引用本文

朱文斌,王玺,葛荣峰.2021.地体的单向和多向聚合与离散[J].地质学报,95(1):124-138.
ZHU Wenbin, WANG Xi, GE Rongfeng.2021. Unidirectional and multidirectional amalgamation-dispersion of terrane[J]. Acta Geologica Sinica,95(1):124-138.

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  • 收稿日期:2020-08-04
  • 最后修改日期:2020-10-03
  • 录用日期:2020-10-12
  • 在线发布日期: 2021-01-25
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