Open AccessEARLY NEOPROTEROZOIC CRUST FORMATON IN THE DZABKHAN MICROCONTINENT, CENTRAL ASIAN OROGENIC BELT
Author(s) -
В. П. Ковач,
И. К. Козаков,
Alfred Kröner,
Е. Б. Сальникова,
KuoLung Wang,
H.-Y. Lee,
SunLin Chung
Publication year - 2017
Publication title -
geodinamika i tektonofizika
Language(s) - English
Resource type - Journals
ISSN - 2078-502X
DOI - 10.5800/gt-2017-8-3-0272
Subject(s) - precambrian , terrane , crust , geology , geochemistry , basement , metamorphic rock , earth science , petrology , paleontology , tectonics , geography , archaeology
The Dzabkhan microcontinent was defined by [Mossakovsky et al., 1994] as a cratonic terrane with an early Precambrian basement that combines highgrade metamorphic complexes of the Songino, Dzabkhan, Otgon, Baidarik, Ider and Jargalant Blocks. However, early Precambrian ages have so far only been recognized in the Baidarik and Ider blocks [Kozakov et al., 2007, 2011; Kröner et al., 2015]