PECULIARITIES OF PRE-CAMBRIAN AND PHANEROZOIC GRANITE-GNEISS STRUCTURE-FORMATION

Authors

  • V. SHEVCHUK
  • V. SHEVCHUK

Abstract

Different style of Archean, Proterozoic and Phanerozoic granite-gneiss structure-formation is argued. It caused by changes of thicknesses, thermal and rheologic regimes of lithosphere. Intermediate character of structural demonstration of Paleoproterozoic granite-formation with development of granite-gneiss monocline have been analyzed.

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Published

2025-01-16

Issue

No. 37 (2006): Visnyk of Taras Shevchenko National University of Kyiv. Geology

Section

Articles

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Copyright (c) 2025 В. ШЕВЧУК, В. ШЕВЧУК

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How to Cite

SHEVCHUK, V. ., & SHEVCHUK, V. . (2025). PECULIARITIES OF PRE-CAMBRIAN AND PHANEROZOIC GRANITE-GNEISS STRUCTURE-FORMATION. Visnyk of Taras Shevchenko National University of Kyiv. Geology, 37, 4-6. https://geology.bulletin.knu.ua/article/view/3363