Results 191 to 200 of about 220,175 (263)

Hydrothermally altered dolerite dykes in East Greenland: implications for Ca-metasomatism of basaltic protoliths

open access: closedContributions to Mineralogy and Petrology, 1994
Dolerite dykes that cut Tertiary baslats near the Skaergaard intrusion, East Greenland, are extensively altered to metasomatic assemblages indicating large scale mobilisation of calcium and alkalis. The alteration is characterised by replacement of the dolerite by prehnite together with lesser amounts of epidote, amphibole, salite, titanite, calcite ...
N. M. Rose, D. K. Bird
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Hydrothermal. Alteration of a Variscian Granite, Magmatic Autometasomatism and Fault Related Vein Metasomatism

open access: closed, 1987
Two types of hydrothermal alteration can be recognized in a biotite granite of Variscan age in Northern Switzerland. The first is related to the intrusion of the granite and lead to the replacement of K-spar and biotite by muscovite, of plagioclase by sericite and calcite and to a chloritization of biotite. This process affected the granite as a whole.
T. J. Peters
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Metasomatism in Iceland: Hydrothermal Alteration and Remelting of Oceanic Crust

open access: closed, 1987
The geochemistry of Icelandic volcanics, especially as pertains LIL-elements, RE-elements, and isotopes, has in the literature called for explanations involving heterogeneous mantle source. These explanations are shown to be incompatible with the data at hand.
S. Steinþórsson   +3 more
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Iron isotope fractionation during fluid metasomatism and ore-forming processes in magmatic-hydrothermal systems

open access: closedGeochimica et Cosmochimica Acta, 2023
Wang Liao   +6 more
openalex   +2 more sources

A fluid inclusion study of the Tourmaline Hill Granite, Umberatana, South Australia: Implications for hydrothermal activity and wallrock metasomatism

open access: closedMineralogy and Petrology, 1987
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
openalex   +3 more sources

Hydrothermal metasomatism of a peralkaline granite pegmatite, Khaldzan Buragtag massif, Mongolian Altai; complex evolution of REE-Nb minerals

open access: closed, 2016
The low-temperature hydrothermal alteration of certain rare-metal minerals is recorded in a quartz-epidote metasomatite from the Tsakhirin Khuduk occurrence in the Khaldzan-Buragtag Nb-REE-Zr deposit, Mongolian Altai. A peralkaline granitic pegmatite was
Bogusław Bagiński   +4 more
openalex   +2 more sources

Mesoproterozoic and Paleozoic hydrothermal metasomatism in the giant Bayan Obo REE-Nb-Fe deposit: Constrains from trace elements and Sr-Nd isotope of fluorite and preliminary thermodynamic calculation

open access: closedPrecambrian Research, 2018
Shang Liu   +8 more
openalex   +2 more sources

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