印度东高止麻粒岩地体Visakhapatnam地区细斑岩地球化学特征

P.V.Nageswara Rao , A.T. Rao , M. Yoshida
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引用次数: 1

摘要

在印度东高加斯麻粒岩地体(EGGT)的Visakhapatnam地区,细粒岩与基性麻粒岩、绿粒岩、钙硅酸盐岩、石英岩和孔达利岩的小带一起赋生。根据地磁关系和地球化学特征,区分了灰色和奶油色瘦铁矿互层型。矿物学和地球化学证据表明,细斑岩属于变质沉积成因。总REE、LREE/HREE和Eu-Eu *数据表明它们来源于太古宙后花岗闪长岩上地壳,其中含有大量富钾花岗质成分的不纯灰岩。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Geochemical characters of leptynites from the Visakhapatnam area in the Eastern Ghats granulite terrane, India

Leptynites occur with minor bands of basic granulites, charnockites, calc-silicate rocks, quartzites and khondalites in the Visakhapatnam area in the Eastern Ghats granulite terrane (EGGT), India. Interbedded grey and cream leptynite types are distinguished based on field relations and geochemistry. The mineralogical and geochemical evidences favour a metasedimentary origin for leptynites. The total REE, LREE/HREE and Eu-Eu data indicate their derivation from the post-Archaean granodioritic upper crust comprising large proportions of impure greywackes with K-rich granitic components.

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