Т. В. Каулина

ORCID: 0000-0002-6530-2187
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About
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Research Areas
  • Geological and Geochemical Analysis
  • Geochemistry and Geologic Mapping
  • earthquake and tectonic studies
  • High-pressure geophysics and materials
  • Geological Studies and Exploration
  • Radioactive element chemistry and processing
  • Geotechnical and Geomechanical Engineering
  • Methane Hydrates and Related Phenomena
  • Paleontology and Stratigraphy of Fossils
  • Geological Formations and Processes Exploration
  • Hydrocarbon exploration and reservoir analysis
  • Mineralogy and Gemology Studies
  • Geochemistry and Elemental Analysis
  • Mining and Gasification Technologies
  • Nuclear materials and radiation effects
  • Geological Modeling and Analysis
  • Marine and environmental studies
  • Planetary Science and Exploration
  • Geomagnetism and Paleomagnetism Studies
  • Astro and Planetary Science
  • Geochemistry and Geochronology of Asian Mineral Deposits

Geological Institute
2014-2024

Kola Science Centre
2015-2024

ORCID
2020

Murmansk State Technical University
2016-2017

Russian Academy of Sciences
2010-2014

Research Article| August 01, 2010 Mesoarchean subduction processes: 2.87 Ga eclogites from the Kola Peninsula, Russia M.V. Mints; Mints 1Geological Institute of Russian Academy Sciences, Moscow 119017, Search for other works by this author on: GSW Google Scholar E.A. Belousova; Belousova 2GEMOC ARC National Key Centre, Department Earth and Planetary Macquarie University, NSW 2109, Australia A.N. Konilov; Konilov L.M. Natapov; Natapov A.A. Shchipansky; Shchipansky W.L. Griffin; Griffin S.Y....

10.1130/g31219.1 article EN Geology 2010-07-13

Abstract The Central Indian Tectonic Zone (CITZ) marks the suture zone where North and South cratonic blocks amalgamated to form Greater Landmass (GIL). It consists of three broad domains from west east: central CITZ occupying region mainland India juxtaposed between two mobile belts, namely Sausar Mobile Belt (SMB) in south Mahakoshal (MMB) north; Chotanagpur Granite Gneiss Complex (CGGC) lying east main CITZ; easternmost Shillong Plateau Gneissic (SPGC). studied granites are Bathani...

10.1144/sp457.11 article EN Geological Society London Special Publications 2017-01-01

Abstract Multidisciplinary studies of zircons, rock-forming minerals and the whole-rock composition granulite samples from Bug Granulite–Gneiss Complex, Ukraine (including ion microprobe REE analysis, secondary mass spectrometry (SIMS) U–Pb laser ablation inductively coupled plasma (LA-ICP-MS) Lu–Hf analysis zircons a single sample) have revealed three major stages in geological evolution complex. (i) At 3.66 Ga, mafic intrusion contaminated with felsic rocks formed, as evidenced by 3.74 Ga...

10.1144/sp449.3 article EN Geological Society London Special Publications 2016-09-30

The Central Indian Tectonic Zone (CITZ) is major E-W trending suture zone between Northern and Southern crustal blocks. southern portion of the CITZ comprises three litho-tectonic units: Tirodi Gneissic Complex (TGC), Sausar Mobile Belt (SMB) Bhandara-Balaghat Granulite (BBGB). Elemental isotopic data are used to constrain genesis granitoids their protoliths, which may help us understand Proterozoic evolution in CITZ. Geochemical results consistent with previous studies that these granitoid...

10.2343/geochemj.gj22016 article EN GEOCHEMICAL JOURNAL 2022-01-01

Recrystallization of zircons under the influence fluids was studied using examples from Precambrian rocks (microcline granites, metasedimentary, and mafic rocks) Kola Peninsula. All zircon crystals showed complex internal textures visible by cathodoluminescence backscattered electron (BSE) imaging. Detailed mineralogical geochemical studies with subsequent secondary ion mass spectrometer U–Pb dating different domains show that texture formation can be interpreted in terms metasomatic...

10.1080/00206814.2014.961976 article EN International Geology Review 2014-10-08

The Kola region (NE of Fennoscandian Shield) has high uranium potential. most promising structures within the in respect to enrichment are Litsa area and Salla-Kuolajarvi zone. principal objective present study was define sequence timing deposition these areas. Isotopic (U-Pb Rb-Sr) exploration rocks from Skal’noe Dikoe U occurrences Ozernoe zone carried out. As it follows isotopic dating, stages mineralization had taken place 2.3–2.2, 1.75–1.65, 0.40–0.38 Ga ago, simultaneously with...

10.3390/min8120563 article EN Minerals 2018-12-01
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