Late Variscan mineralizing systems related to orogenic processes: The French Massif Central

被引:88
作者
Bouchot, V [1 ]
Ledru, P [1 ]
Lerouge, C [1 ]
Lescuyer, JL [1 ]
Milesi, JP [1 ]
机构
[1] Bur Rech Geol & Minieres, F-45060 Orleans, France
关键词
orogenic gold; tungsten; tin; rare-metals; mineralizing system; Phanerozoic; Variscan belt; French Massif Central;
D O I
10.1016/j.oregeorev.2005.07.017
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The French Massif Central constitutes an exceptional study area due to the diversity of its metallic deposits, its internal position in the Variscan belt, and the abundance of available geological, geophysical and metallogenic data obtained within the GeoFrance 3D Programme. The deposits, formed towards the end of the orogenic evolution, represent the economic products of two distinct mineralizing systems, a Au +/- Sb hydrothermal system and a W +/- Sn and rare-metals magmatic-hydrothermal system, which were simultaneously active during a short time span between ca. 3 10 and 300 Ma. Two types of gold deposit can be distinguished on the basis of their depth of emplacement: "deep-seated" gold deposits developed under lithostatic to hydrostatic pressure during rapid exhumation, and "shallow" gold deposits emplaced under hydrostatic pressure with no significant uplift. Deposits of W +/- Sn and rare-metals were emplaced in the upper crust during final crystallization of specialized magmas after their rapid ascent, perhaps enhanced by simultaneous regional uplift. The gold-bearing systems are associated with a complex network of re-activated crustal-scale faults initially active during the period between 335 and 315 Ma. Normal motion along the faults, coeval with 335 to 315 Ma granite-migmatite domes, played a major role in the 3D distribution of the hydrothermal plumbing system. Gold and related metals were carried within huge hydrothermal cells, which reached ca. 100 kin by 10 km in area, and 30 kin in depth. In contrast, granites rich in magmatophile elements (W, Sri, rare-metals) generated smaller hydrothermal cells (10 km by 10 kin in area, and <6 km deep). Extraction of metals, by both deep-seated fluids and specialized magmas, occurred during granulitization of the lower crust at 300 +/- 15 Ma. In the French Massif Central, the genesis of the two late Carboniferous mineralizing systems coincided with the end of syn-collisional extension and ended just before post-collisional extension. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码:169 / 197
页数:29
相关论文
共 126 条
  • [1] AISSA M, 1987, ECHASSIERES FORAGE S, V1, P335
  • [2] ALEXANDROV P, 2000, THESIS NANCY U
  • [3] ALIKOUSS S, 1993, BRITTLEDUCTILE TRANS
  • [4] [Anonymous], 1978, Z DTSCH GEOL GES
  • [5] ARTHAUD F, 1977, GEOL SOC AM BULL, V88, P1305, DOI 10.1130/0016-7606(1977)88<1305:LPSFIS>2.0.CO
  • [6] 2
  • [7] AUGAY JF, 1979, THESIS LYON U
  • [8] BARBEY L, 1993, J FRANCAISES MINERAL, V5, P28
  • [9] BELKASMI M, 1991, P 2K YEARS SGA M SOU, V25, P729
  • [10] The Biards Sb-Au-bearing shear zone (Massif Central, France): An indicator of crustal-scale transcurrent tectonics guiding late Variscan collapse
    Bellot, JP
    Lerouge, C
    Bailly, L
    Bouchot, V
    [J]. ECONOMIC GEOLOGY AND THE BULLETIN OF THE SOCIETY OF ECONOMIC GEOLOGISTS, 2003, 98 (07): : 1427 - 1447