Geochronological evidence for existence of South Mongolian microcontinent - A zircon U-Pb age of grantoid gneisses from the Yagan-Onch Hayrhan metamorphic core complex

Chinese Science Bulletin

Volumn 46, Issue 23, 2001, Pages 2005-2008

  Wang, Tao ^a   Zheng, Yadong ^a   Gehrels, G E ^b   Mu, Zhiguo ^a  

^a PEKING UNIVERSITY   (China)

^b UNIVERSITY OF ARIZONA   (United States)

Author keywords

Gniesses; Proterozoic; South Mongolian microcontinent; Zircon U Pb age

Indexed keywords

LEAD; ZIRCONIUM;

ARTICLE; GEOCHEMICAL ANALYSIS; GEOLOGICAL ERA; MONGOLIA; PROTEROZOIC; ROCK;

EID: 0035674360     PISSN: 10016538     EISSN: None     Source Type: Journal    
DOI: 10.1007/BF02901917     Document Type: Article

References (9)

1. The south Mongolian Variscan fold system
2. Tectonics of old structures and phosphates of Mongolia
3. Occurrence, age, and implication of the Yangan-Onch Hayrhan metamorphic core complex, southern Mongolia
4. The Yagan metamorphic core complex and extensional detachment fault in Inner Mongolia
5. An enormous thrust nappe and extensional metamorphic core complex newly discovered in Sino-Mongolian boundary area
6. Great Jurassic thrust sheets in Beishan (North Mountains)-Gobi areas of China and southern Mongolia
7. Reconnaissance geology and U-Pb geochronology of the western flank of the coast mountains between Juneau and Skagway, southeastern Alaska
8. Paleozoic sedimentary basins and volcanic-arc system of southern Mongolia