[1]周 洁,李三忠,索艳慧.2019.碰生型微地块的分类及其形成机制.大地构造与成矿学,43(4):795-823.doi:10.16539/j.ddgzyckx.2019.04.012
 ZHOU Jie,LI Sanzhong,SUO Yanhui.2019.Type and Genetic Mechanism of Collision-derived Micro-blocks.Geotectonica et Metallogenia,43(4):795-823.doi:10.16539/j.ddgzyckx.2019.04.012
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碰生型微地块的分类及其形成机制
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2019年43卷04期
页码:
795-823
栏目:
微板块构造专辑
出版日期:
2019-08-15

文章信息/Info

Title:
Type and Genetic Mechanism of Collision-derived Micro-blocks
文章编号:
1001-1552(2019)04-0795-029
作者:
周 洁12 李三忠12* 索艳慧12 李玺瑶12 郭玲莉12 朱俊江12 刘永江12 王光增12 李 阳12
1.海底科学与探测技术教育部重点实验室, 中国海洋大学 海洋高等研究院和海洋地球科学学院, 山东 青岛 266100; 2.青岛海洋科学与技术国家实验室 海洋矿产资源评价与探测技术功能实验室, 山东 青岛 266237
Author(s):
ZHOU Jie12 LI Sanzhong12* SUO Yanhui12 LI Xiyao12 GUO Lingli12 ZHU Junjiang12 LIU Yongjiang12 WANG Guangzeng12 and LI Yang12
1.Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, Institute for Advanced Ocean Study and College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China; 2.Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, Shandong, China
关键词:
微地块 碰撞造山带 板内 洋内 碰撞方式
Keywords:
micro-block collision orogenic belts intra-plate intra-oceanic collisional process
分类号:
P542
DOI:
10.16539/j.ddgzyckx.2019.04.012
文献标志码:
A
摘要:
碰生型微地块是指受大陆碰撞造山作用触发的相对独立的微小板块或地块。本文通过具体实例从多角度对碰生型微地块进行了分类: 按发生碰撞的两侧陆壳性质, 可分为陆-陆、弧-陆和弧-弧碰生型微地块; 按碰撞方式, 可分为追尾式、侧向式、错车式和拥堵式碰生型微地块; 根据微地块本身的物质组成, 可分为碰生型微洋块和碰生型微陆块。总结了碰生型微地块的形成机制——远程碰撞触发模型: 碰撞事件及其远程效应, 触发了地幔内部热结构的非稳定性, 使板块内部的应力失稳, 在大陆内部形成岩石圈尺度的断裂, 大块体被分裂为多个刚性块体, 并发生差异性裂解、逃逸、挤出、旋转等, 形成具有独立运动学特征的微陆块; 在大洋内触发了洋中脊拓展式、跃迁式生长, 形成独立微洋块。碰生型微地块类型划分为研究碰撞造山的非相邻地质体之间的盆-山效应奠定了基础, 为研究“板内”变形机制提供了新依据、新思路。碰生型微洋块的形成记录了大陆碰撞事件的起始时间, 是对基于大陆地质研究而确定的碰撞时间的重要补充。
Abstract:
The collision-derived micro-block is a relatively independent microplate or microblock formed in continental collision or orogeny.In this paper, the collision-derived micro-block is defined from various aspects with specific examples.It can be divided into continent-continent, continent-arc and arc-arc collision-derived micro-blocks according to the colliding continental crust on both sides of the collisional zones; it can also be divided into the rear-end collision, lateral collision, rubbing collision and congestion collision-derived micro-blocks regarding the collisional processes.It can also be divided into collision-derived oceanic micro-block and collision-derived continental micro-block according to the crustal type of the mico-block.Then, this paper summarizes the formation mechanism of the collision-derived micro-block — remote-collision triggering model: the collision event and its remote effect triggered the instability of the mantle thermal structure, resulting in the stress instabilities that destroy the original structure of the lithosphere and form lithosphere-scale fault inside the continent, and the large-scale block is rifted into several rigid micro-blocks.Subsequently, the independent micro-blocks are formed in the kinematics with differential rifting, escape and extrusion.Similarly, in the ocean, the collision event and its remote effect can trigger the jumping and propagation of the mid-ocean ridge, and forming the independent oceanic micro-block.The type division of the collision-derived micro-block is a key for studying complex collisional zones or orogenic belts, and providing theoretical support for refined tectonic research.The formation of the collision-derived micro-block records the starting time of the collision event, which can be an important supplement to the collision time determined by the study of the continental geology.

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备注/Memo

备注/Memo:
收稿日期: 2018-08-29; 改回日期: 2018-11-23
项目资助: “全球变化与海气相互作用”专项(GASI-GEOGE-01)、山东省-国家自然科学基金联合基金(U1606401)、国家重点研发项目(2016YFC0601002、2017YFC0601401)和试采海底孔隙压力监测与海洋物理环境研究项目( 2018c-03-186)联合资助。
第一作者简介: 周洁(1988-), 女, 博士, 主要从事构造地质学研究。Email: zj888@ouc.edu.cn
通信作者: 李三忠(1968-), 男, 教授, 主要从事构造地质学和海洋地质学研究。Email: sanzhong@ouc.edu.cn
更新日期/Last Update: 2019-08-15