Derivation of P–T paths for Middle–Late Triassic very low-grade metapelite from Hongcan Well 1 in the Zoigê Depression and their tectonic implications-Reference-Cited by-同舟云学术

Derivation of P–T paths for Middle–Late Triassic very low-grade metapelite from Hongcan Well 1 in the Zoigê Depression and their tectonic implications

Published:2013-12-31 Issue:1 Volume:59 Page:82-99
ISSN:1001-6538
Container-title:Chinese Science Bulletin
language:en
Short-container-title:Chin. Sci. Bull.

Author:

Tang Yan,Sang Longkang,Liu Rong,Yuan Yanming,Yang Yunlong,Qi Xianmao,Tan Jing

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://link.springer.com/content/pdf/10.1007/s11434-013-0051-2.pdf

Reference49 articles.

1. England PC, Thompson AB (1984) Pressure–temperature–time paths of regional metamorphism I: heat transfer during the evolution of regions of thickened continental crust. J Petrol 25:894–928

2. Spear FS (1993) Metamorphic phase equilibria and pressure–temperature–time paths. Mineralogical Society of America, Washington, DC, pp 19–799

3. Brown M (2010) Paired metamorphic belts revisited. Gondwana Res 18:46–59

4. Powell R, Holland T (2010) Using equilibrium thermodynamics to understand metamorphism and metamorphic rocks. Elements 6:309–314

5. Massimiliano T, Jibamitra G (2010) Garnet compositions as recorders of P–T–t history of metamorphic rocks. Gondwana Res 18:138–146

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1. Provenance of Middle to Late Triassic sedimentary rocks in the Zoige Depression in the NE part of the Songpan-Ganzi Flysch Basin: Petrography, heavy minerals, and zircon U-Pb geochronology;Geological Journal;2017-08-30