Tabiiy fanlar

SPREAD OF ROCKS IN THE MALGUZAR MOUNTAINS

subvolcanic formations, small intrusions, dikes, gabbro-dolerites, gabbro-diabases, diabases, dike belt, rift zone, differentiation, cumulates, geodynamics, Malguzar, Southern Tien Shan

Authors

The Molguzar Mountains are a southeastern continuation of the Northern Nuratau Range and are composed of Lower and Middle
Paleozoic sedimentary-metamorphic rocks. In these deposits, small intrusions and dikes of gabbro-diabase silos, dikes, numerous
diorites, quartz diorites, granodiorites, granite-porphyries, and lamprophyres of the Middle Silurian period are revealed. These
formations are distributed from the Molguzar Mountains through the Northern and Southern Nuratau ranges to the Auminzatau
Mountains and are characterized by manifestations of gold mineralization. Hypabyssal acidic magmatic formations form thermal
fields and vein mineralization, contributing to the circulation of fluids and hydrothermal solutions. These mineralized zones have
been identified in many areas of the study area