Introduction and commentary on ocean plate stratigrapgy

FENG Yimin; ZHANG Yue

2018 Vol. 37, No. 4

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FENG Yimin, ZHANG Yue. Introduction and commentary on ocean plate stratigrapgy[J]. Geological Bulletin of China, 2018, 37(4): 523-531.

Citation:

FENG Yimin, ZHANG Yue. Introduction and commentary on ocean plate stratigrapgy[J]. Geological Bulletin of China, 2018, 37(4): 523-531.

Introduction and commentary on ocean plate stratigrapgy

Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, Shaanxi, China

Received Date: 07 July 2017

Revised Date: 18 March 2018

Publish Date: 25 April 2018

Abstract

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 environment, and structural features of OPS. On such a basis, this paper discusses the role of OPS in regional geological and resources survey. 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.
- ocean plate stratigraphy /
- subduction accretional complex /
- ophiolite /
- ophiolite melange

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References

[1]	Isozaki Y, Maruyama S, Fukuoka F. Accreted oceanic materials in Japan[J]. Tectonophysics, 1990, 181:179-127. doi: 10.1016/0040-1951(90)90016-2 CrossRef Google Scholar
[2]	Wakita K, Metcalfe I. Oceanic Plate Stratigraphy in East and Southeast Asia[J]. Journal of Asia Earth Sciences, 2005, 24:679-702. doi: 10.1016/j.jseaes.2004.04.004 CrossRef Google Scholar
[3]	Kusky T M, Weindley B F. Safonova I. Recognition of Ocean Plate Stratigraphy in accretionary orogens through Earth history:A record of 3.8 billion years of sea floor spreading, subduction, and accretion[J]. Gondwana Research, 2013, 24:501-547. doi: 10.1016/j.gr.2013.01.004 CrossRef Google Scholar
[4]	张克信, 何卫红, 徐亚东, 等.中国洋板块地层分布及构造演化[J].地学前缘, 2016, 23:1-7. Google Scholar
[5]	Yildirim D, Harald F. Ophiolite genesia and global tectonics:Geochemical and tectonic fingerprinting of ancient oceanic lithosphere[J]. GSA Bulletin, 2011, 123(3/4):387-411. Google Scholar
[6]	冯益民, 何世平.祁连山大地构造与造山作用[M].北京:地质出版社, 1996. Google Scholar
[7]	李荣社, 计文化, 杨永成, 等.昆仑山及邻区地质[M].北京:地质出版社, 2008. Google Scholar
[8]	张国伟, 郭安林, 王岳军, 等.中国华南大陆构造与问题[J].中国科学:地球科学, 2013, 56:1804-1826. Google Scholar
[9]	潘桂棠, 肖庆辉, 陆松年, 等.中国大地构造单元划分[J].中国地质, 2009, 36(1):1-28. Google Scholar
[10]	潘桂棠, 肖庆辉.中国大地构造图(1:2500000)[M].北京:地质出版社, 2015. Google Scholar
[11]	潘桂棠, 陆松年, 肖庆辉, 等.中国大地构造阶段划分和演化[J].地学前缘, 2016, 23:1-23. Google Scholar
[12]	徐学义, 李向民, 王洪亮, 等. 1:1000000祁连山及邻区成矿地质背景图(附说明书)[M].北京:地质出版社, 2008. Google Scholar
[13]	袁学诚, 林隆栋, 许乐红.再论无机生油假说及中国找油前景[J].中国地质, 2017, 44(3):473-484. Google Scholar
[14]	Song S G, Feng Y M. Subduction complex beilt and their tectonic implication, North Qilian mountains[J]. Acta Geoscientia Sinica, 1996, Special Issue:6-9. Google Scholar
[15]	吴汉泉, 宋述光. 北祁连山两种类型蓝片岩及其构造特征[C]//现代地质研究文集(上). 南京: 南京大学出版社, 1992. Google Scholar
[16]	Wu H Q, Feng Y M, Song S G. Metamorphic, deformation of blueschist belts and their implications in North Qilian Mountains, China[J]. J. Metamorphic Geol., 1993, 11:523-536. doi: 10.1111/jmg.1993.11.issue-4 CrossRef Google Scholar
[17]	Liou J G, Graham S A, Maruyama S, 等. 中国西部元古代蓝片岩带—世界前寒武纪蓝片岩的最佳论据[C]//肖序常, 汤耀庆. 古中亚复合巨型缝合带南缘构造演化. 北京: 科学技术出版社, 1991: 1-125. Google Scholar