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Synsedimentary faulting and sediment hosted submarine hydrothermal mineralization in the late Palaeozoic Rhenish basin (Germany)

Viac o knihe

Under both structural and mineral-exploration aspects this work deals with the reconstruction of synsedimentary fault system which were active during the development of the Rhenish Basin in the Devonian and Lower Carboniferous. The Rhenish Massif (Germany) is a good test case for studying the spatial, temporal and genetic relationships between synsedimentary fault activities and submarine-hydrothermal mineralization.

Nákup knihy

Synsedimentary faulting and sediment hosted submarine hydrothermal mineralization in the late Palaeozoic Rhenish basin (Germany), Wolfgang Werner

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Rok vydania
1989
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