Chemical and Mineralogical Composition of Water-Bearing Materials of the Kuldur Geothermal Reservoir (Jewish Autonomous Region)

This article provides results of mineralogical and geochemical studies of granodiorites of the Kuldur low-mineralized thermal water reservoir. The site of geological and groundwater studies belongs to the Pionerskii massif located within the Lesser Khingan block of the Bureya compoite terrain. Grani...

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Bibliographic Details
Published in:IOP conference series. Earth and environmental science 2020-04, Vol.459 (4), p.42038
Main Authors: Lyamina, L A, Kharitonova, N A, Karabtsov, A A
Format: Article
Language:English
Subjects:
Bearing materials
Chemical composition
Cratons
Groundwater
Groundwater studies
Massifs
Mesozoic
Mineralogy
Paleozoic
Reservoirs
Thermal water
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Summary:This article provides results of mineralogical and geochemical studies of granodiorites of the Kuldur low-mineralized thermal water reservoir. The site of geological and groundwater studies belongs to the Pionerskii massif located within the Lesser Khingan block of the Bureya compoite terrain. Granitoids of the Tyrma-Bureya assemblage in the Pionerskii massif are considered to have formed in the early Mesozoic era, not in the late Paleozoic era, as deemed before. Granitoids of the assemblage under study were likely formed in the geodynamic backdrop of the collision of the North Asian and Sino-Korean cratons.
ISSN:1755-1307
1755-1315
DOI:10.1088/1755-1315/459/4/042038