Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Nicholas H. S. Oliver"'
Autor:
Brian Thomson, Warren T. Pratt, David A. Rhys, Nicholas H. S. Oliver, Scott W. Halley, Peter Fischl, Vyacheslav V. Akinin, Dotzo Dotzov
Publikováno v:
Economic Geology. 118:93-122
The Kupol epithermal Au-Ag vein district is located in the northern part of the Okhotsk-Chukotka volcanic belt, a Late Cretaceous subduction-related continental volcanic arc exposed for >3,000 km along the eastern coast of Russia. High-grade veins ar
Publikováno v:
Journal of Petrology. 35:1455-1491
Publikováno v:
Journal of Metamorphic Geology. 12:197-206
A breccia vein sampled from a shear zone in greenschist facies metapelites at Mount Isa, Queensland, Australia, shows a systematic variation in vein geometry that is related to the geometry of folding and faulting within the sample. Calcite vein-fill
Publikováno v:
Journal of Metamorphic Geology. 11:705-720
Large calcite veins and pods in the Proterozoic Corella Formation of the Mount Isa Inlier provide evidence for kilometre-scale fluid transport during amphibolite facies metamorphism. These 10- to 100-m-scale podiform veins and their surrounding alter
Autor:
Thomas C. Hoering, Nicholas H. S. Oliver, Wayne C. Shanks, Timothy W. Johnson, Douglas Rumble
Publikováno v:
Geochimica et Cosmochimica Acta. 56:4257-4265
Sulfur isotope ratios of pyrite (py) and pyrrhotite (po) from regionally metamorphosed graphitic sulfidic schists and related rocks from south-central Maine, USA, were analysed using SO2 and SF6 techniques. There is a broad range in δ34S values for
Autor:
Ian Cartwright, Nicholas H. S. Oliver
Publikováno v:
Journal of the Geological Society. 149:693-696
Marbles adjacent to the Burstall granite, Mary Kathleen, Australia, record up-temperature fluid flow during contact metamorphism. These fluids were water-rich and probably partially derived from devolatilization reactions. By contrast, Fe-rich skarns
Publikováno v:
Contributions to Mineralogy and Petrology. 111:94-112
Unaltered metasediments of the Mary Kathleen Fold Belt are composed predominantly of layered amphibolite-facies scapolitic calc-silicate rocks in which minimal infiltration of externally derived fluids occurred during regional metamorphism. There wer
Publikováno v:
Mineralium Deposita. 50:1031-1031
Publikováno v:
Mineral Deposit Research: Meeting the Global Challenge ISBN: 9783540279457
Ernest Henry is an iron oxide-copper-gold deposit characterized by magnetite≫hematite, chalcopyrite as the only significant hypogene copper mineral. It occurs within a large, zoned, medium to high temperature alteration system. Pre- to synmineraliz
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::492388c5868cc4c5a33d0a1ad8e6d046
https://doi.org/10.1007/3-540-27946-6_200
https://doi.org/10.1007/3-540-27946-6_200
Publikováno v:
Australian Journal of Earth Sciences. 42:231-232