Fluid inclusions and sulphur isotopes of the Valea Morii ore deposit (Apuseni mountains, Romania):: telescoping between porphyry and low-sulfidation epithermal ore deposits?

被引：3

作者：

André-Mayer, AS

Leroy, JL

Marcoux, É

Lerouge, C

机构：

[1] Univ Henri Poincare, UMR G2R, F-54506 Vandoeuvre Les Nancy, France

[2] Univ Orleans, ISTO, F-45072 Orleans 2, France

[3] Bur Rech Geol & Minieres, REM MESY, F-45060 Orleans 2, France

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES | 2001年 / 333卷 / 02期

关键词：

Apuseni mountains; Romania; epithermal; porphyry copper; deposit; fluids; telescoping;

D O I：

10.1016/S1251-8050(01)01611-1

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

The Valea Morii Cu-Au ore deposit (Apuseni mountains, Romania) is characterised by a spatial association of a porphyry copper (Cu +/- Au) with a low-sulfidation epithermal deposit (Au). Microthermometric and sulphur isotopic data, obtained on both porphyry and epithermal veins, express a telescoping between these two types of mineralization, which can be explained either by an erosion phenomenon during the hydrothermal activity or by a collapse of the upper part of the hydrothermal system. (C) 2001 Academie des sciences/Editions scientifiques et medicales Elsevier SAS.

引用

页码：121 / 128

页数：8

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