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大洋板块地层(OPS)简介及评述

冯益民 张越

地质通报2018,Vol.37Issue(4):523-531,9.
地质通报2018,Vol.37Issue(4):523-531,9.

大洋板块地层(OPS)简介及评述

Introduction and commentary on ocean plate stratigrapgy

冯益民 1张越1

作者信息

  • 1. 中国地质调查局西安地质调查中心,陕西西安710054
  • 折叠

摘要

Abstract

The concept of ocean plate stratigraphy was proposed by Japanese geologist Isozaki Y and some other experts in 1990.OPS is a tectonic-sedimentary sequence,which is set up by ocean plate movement from oceanic ridge to sea trench.Research on OPS has gained remarkably progress,which has enriched the meaning of OPS.This paper introduces basic concept,components,formation en-vironment,and structural features of OPS.On such a basis,this paper discusses the role of OPS in regional geological and resources sur-vey.It is preliminarily suggested that subduction accretional complex(SAC)should be used in place of'ocean plate stratigraphy'in the study of orogenic belt.As'stratigraphy'is not genetically equivalent to 'complex',the SAC is better than the OPS in usage.

关键词

大洋板块地层/俯冲增生杂岩/蛇绿岩/蛇绿混杂岩

Key words

ocean plate stratigraphy/subduction accretional complex/ophiolite/ophiolite melange

分类

天文与地球科学

引用本文复制引用

冯益民,张越..大洋板块地层(OPS)简介及评述[J].地质通报,2018,37(4):523-531,9.

基金项目

中国地质调查局项目《祁连成矿带肃南—大柴旦地区地质矿产调查》(编号:DD20160012) (编号:DD20160012)

地质通报

OA北大核心CSCDCSTPCD

1671-2552

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