Mass balance during retrogression of eclogite-facies minerals in the;Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China

	Mass balance during retrogression of eclogite-facies minerals in the;Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China
	Yang, TN 3; Xu, ZQ ; Leech, M
刊名	AMERICAN MINERALOGIST
	2004
卷号	89 期号:10 页码:1525-1532
ISSN号	0003-004X
英文摘要	Eclogite from Rongcheng in the easternmost part of the Sulu ultrahigh-pressure metamorphic terrane has broken down (at least partially) with the formation of coronae of spinel + anorthite around kyanite, symplectites of pargasite + plagioclase around garnet, and symplectites of diopside + plagioclase after omphacite. Textural evidence and microprobe analysis indicate that this breakdown was generated by discontinuous reactions. Quantification of material transfer and textural information suggest that the reaction mechanism involved local exchange of components among the three major minerals (omphacite, garnet, and kyanite) during dissolution and discontinuous precipitation, coupled with exchange between eclogites and their host rocks. The symplectite formed after omphacite gained Al and minor Si and Na from its surroundings, and lost Mg, Ca, and minor Fe to its surroundings. Formation of the symplectite around garnet was accompanied by gain of Ca, Al, Si, Na, and H(2)O, and by loss of Mg and Fe(2+) to its surroundings. Coronae around kyanite gained Ca, Fe, Mg, and minor Si, and provided Al to their surroundings. Material exchange between eclogite and host rocks occurred as well: eclogite gained minor Al, Na, and H(2)O from the host rocks, and provided Mg, Fe, and Ca to the host rocks. Pressure and temperature estimation using THERMOCALC yielded a lower temperature (655 +/- 70 degreesC) and higher pressure (1.3 +/- 0.2 GPa), which values contrast with estimates made by other authors. Strong deformation may have created a path for ingress of hydrous fluids, then resulted in a localized lower T and/or higher P.
学科主题	变质岩岩石学
WOS关键词	METAMORPHIC ROCKS ; BEARING ECLOGITE ; LU REGION ; COESITE ; OLIVINE ; PLAGIOCLASE ; OMPHACITE ; DIFFUSION ; PETROLOGY ; TEXTURES
WOS研究方向	Geochemistry & Geophysics ; Mineralogy
语种	英语
出版者	MINERALOGICAL SOC AMER
WOS记录号	WOS:000224509500022
内容类型	期刊论文
源URL	[http://119.78.100.197/handle/2HKVOGP0/37747]
专题	中国地质科学院地质研究所
作者单位	1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China. 2.Stanford Univ, Stanford, CA 94305 USA. 3.中国地质科学院地质研究所
推荐引用方式 GB/T 7714	Yang, TN,Xu, ZQ,Leech, M. Mass balance during retrogression of eclogite-facies minerals in the;Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China[J]. AMERICAN MINERALOGIST,2004,89(10):1525-1532.
APA	Yang, TN,Xu, ZQ,&Leech, M.(2004).Mass balance during retrogression of eclogite-facies minerals in the;Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China.AMERICAN MINERALOGIST,89(10),1525-1532.
MLA	Yang, TN,et al."Mass balance during retrogression of eclogite-facies minerals in the;Rongcheng eclogite, eastern Sulu ultrahigh-pressure terrane, China".AMERICAN MINERALOGIST 89.10(2004):1525-1532.