史密斯地层与非史密斯地层

张克信; 殷鸿福; 朱云海; 王国灿; 冯庆来; 龚一鸣

Volume 28 Issue 4

Jul. 2003

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Article Navigation > Earth Science > 2003 > 28(4): 361-369

ZHANG Ke-xin, YIN Hong-fu, ZHU Yun-hai, WANG Guo-can, FENG Qing-lai, GONG Yi-ming, 2003. Smith Strata and Non-Smith Strata. Earth Science, 28(4): 361-369.

Citation:

ZHANG Ke-xin, YIN Hong-fu, ZHU Yun-hai, WANG Guo-can, FENG Qing-lai, GONG Yi-ming, 2003. Smith Strata and Non-Smith Strata. Earth Science, 28(4): 361-369.

ZHANG Ke-xin, YIN Hong-fu, ZHU Yun-hai, WANG Guo-can, FENG Qing-lai, GONG Yi-ming, 2003. Smith Strata and Non-Smith Strata. Earth Science, 28(4): 361-369.

Citation:

ZHANG Ke-xin, YIN Hong-fu, ZHU Yun-hai, WANG Guo-can, FENG Qing-lai, GONG Yi-ming, 2003. Smith Strata and Non-Smith Strata. Earth Science, 28(4): 361-369.

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Smith Strata and Non-Smith Strata

Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2003-04-18
Publish Date: 2003-07-25

Abstract

Abstract

International Stratigraphic Guide pointed out that stratigraphy should be defined as the description of all rock bodies constituting the earth crust. Hence, all kinds of rocks, including sedimentary, igneous, metamorphic, solidified and unsolidified rocks, should be considered as research contents of stratigraphy. While traditional stratigraphy mainly studies strata by gravitative deposit, though including some parts of bedded volcanic rocks such as lava, pyroclastic rocks and volcanic ashes. Smith strata are regarded as the strata deposited in gravity, including related strata such as depositional metamorphic and volcanic rocks in this paper. Whereas in modern stratigraphy, the mechanic mechanism of strata origination includes not only gravity, but also thermal (ophiolite), mechanic and tectonic forces (orogenic mixtite and tectonite). In these above-mentioned non-gravitative conditions, the strata, formed with their own mechanisms but not with the overlap rules of Smith stratigraphy, are called non-Smith strata here. In the orogenic belt mélange regions, formations of non-Smith strata could be classified into subduct-scrape-match, subduct-return-match and subduct-overthrust types.
- modern stratigraphy,
- Smith strata,
- non-Smith strata,
- mechanism,
- orogenic belt mélange

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References(22)

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