Results 181 to 190 of about 210,813 (245)
The Ag-Pb-Zn ore deposit at the Elura mine, New South Wales, Australia, is situated in a Devonian slate belt and essentially consists of two vertically elongated, ellipsoidal bodies of massive sulfide.
J. A. de Roo
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We report new compositional and textural observations on amphiboles hosted in oceanic gabbros recovered from the slow spreading Mid‐Atlantic (MARK area) and Southwest Indian (Hole 735B) ridges and the fast spreading East Pacific Rise (Hess Deep) in an ...
K. M. Gillis, Peter S Meyer
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Homogenization temperatures and salinity data are documented for fluid inclusions present in quartz from a Palaeozoic alkaline to peralkaline granite intrusion. A wide range of salinities (3.8 to 60.6 wt% NaCl equivalent) and homogenization temperatures (25.8 to 537 °C) indicates a sequential entrapment of different fluids, whereby the detected ...
Bernd G. Lottermoser
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Chen Ji, Kai‐Jun Zhang, Lilong Yan
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Geochimica et Cosmochimica Acta, 1998
Abstract Wollastonite ores and garnet-pyroxene skarns in the Willsboro-Lewis district, New York, USA were formed in a complex hydrothermal system associated with the emplacement of a large anorthosite pluton. Contact-metamorphic marbles were replaced by wollastonite, garnet, and clinopyroxene during infiltration metasomatism involving large volumes ...
James F. Olmsted, Philip R. Whitney
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Abstract Wollastonite ores and garnet-pyroxene skarns in the Willsboro-Lewis district, New York, USA were formed in a complex hydrothermal system associated with the emplacement of a large anorthosite pluton. Contact-metamorphic marbles were replaced by wollastonite, garnet, and clinopyroxene during infiltration metasomatism involving large volumes ...
James F. Olmsted, Philip R. Whitney
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The Role of Hydrogen - Metasomatism in the Hydrothermal Kaolin Occurrences, Gönen, Western Turkey
Ş. Ali Sayin
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Abiogenic structures, formed by fluid emission in subaerial mud pools and nearby stromatolites, from stratigraphically related carbonate sediments, occur in the southern part of the approximately 3.3 to 3.5-b.y.-old Barberton greenstone belt.
Maarten J. de Wit+3 more
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