Limits of hydrosphere-lithosphere interaction: Origin of the lowest-known δ18O silicate rock on Earth in the Paleoproterozoic Karelian rift

Geology

Volumn 38, Issue 7, 2010, Pages 631-634

  Bindeman, I N ^a   Schmitt, A K ^b   Evans, D A D ^c  

^a UNIVERSITY OF OREGON   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

^c YALE UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EARTH CLIMATE; HYDROTHERMALLY; METEORIC WATERS; OXYGEN ISOTOPIC; PALEOGEOGRAPHIC RECONSTRUCTION; PALEOPROTEROZOIC; PLATE TECTONICS; POLAR REGIONS; PROTOLITHS; RIFT ZONES; SILICATE ROCKS; TEMPERATURE GRADIENT; WATER ROCK INTERACTIONS;

DISTILLATION; GALLIUM; IGNEOUS ROCKS; ISOTOPES; OCEANOGRAPHY; OXYGEN; PHOSPHATE MINERALS; RESERVOIRS (WATER); ROCKS; SEAWATER; SILICATE MINERALS; TECTONICS;

EARTH (PLANET);

GEOCHRONOLOGY; GEOLOGICAL RECORD; HYDROSPHERE; HYDROTHERMAL ALTERATION; LITHOSPHERE; METASEDIMENT; METAVOLCANIC ROCK; OXYGEN ISOTOPE; PALEOCEANOGRAPHY; PALEOCLIMATE; PALEOGEOGRAPHY; PALEOTEMPERATURE; PRECIPITATION (CLIMATOLOGY); PROTEROZOIC; PROTOLITH; SILICATE; TEMPERATURE GRADIENT; WATER-ROCK INTERACTION;

KARELIA [(ADS) RUSSIAN FEDERATION]; RUSSIAN FEDERATION;

EID: 77956048496     PISSN: 00917613     EISSN: 00917613     Source Type: Journal    
DOI: 10.1130/G30968.1     Document Type: Article

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