Some problems in the research of adakite

ZHU Di-cheng; PAN Gui-tang; DUAN Li-ping; XIA Lin; LIAO Zhong-li; WANG Li-quan

Northwestern Geology > 2003 > 36(2): 13-19.

ZHU Di-cheng, PAN Gui-tang, DUAN Li-ping, et al. Some problems in the research of adakite[J]. Northwestern Geology, 2003, 36(2): 13-19.

Citation:

ZHU Di-cheng, PAN Gui-tang, DUAN Li-ping, et al. Some problems in the research of adakite[J]. Northwestern Geology, 2003, 36(2): 13-19.

Citation:

ZHU Di-cheng, PAN Gui-tang, DUAN Li-ping, et al. Some problems in the research of adakite[J]. Northwestern Geology, 2003, 36(2): 13-19.

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Some problems in the research of adakite

1.
Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China;China University of Geosciences, Beijing 100083, China
2.
Chengdu Institute of Geology and Mineral Resources, Chengdu 610082, China
3.
China University of Geosciences, Beijing 100083, China

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Received Date: February 19, 2003
Revised Date: April 14, 2003
Published Date: June 04, 2003

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Abstract

Abstract

Based on the analysis for the state in the research of adakite in China, this paper discusses the major advances in the research of adakite, and probes in to the particular geodynamic significances that are less or out of noticed before.This paper emphasizes that O-type adakite may be as an indicator to reveal the start of oceanic shrink and subduction, whereas the C-type adakite maybe indicate that the crust has thickened before the forming of this kind of magma.And then, the authors point out that many problems of adakite may be resolved by studying the adakite in Tibetan Plateau.
- adakite,
- oceanic shrink and subduction,
- crust thickened,
- geodynamic significances,
- Tibetan Plateau

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References (25)

References

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