Premium
The Characteristics and Its Geological Significance of Fluid Inclusions in Yingchengzi Gold Deposit, Heilongjiang Province
Author(s) -
CHAI Peng,
SUN Jinggui,
GU A'lei,
ZHAO Keqiang
Publication year - 2014
Publication title -
acta geologica sinica ‐ english edition
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 61
eISSN - 1755-6724
pISSN - 1000-9515
DOI - 10.1111/1755-6724.12375_5
Subject(s) - chai , chinese academy of sciences , library science , archaeology , history , theology , philosophy , china , computer science
The Yingchengzi gold deposit is located in Shalai town, Ning'an county, Mudanjiang City, Southeast Heilongjiang Province, in the continental margin of NE China (Sun et al. 2013), tectonically on the east end of the Central Asia Orogenic Belt (CAOB), so called Zhangguangcai Range, adjacent to the Jiamusi Massifs in the northeast, the North China Plate in the south, and the Songliao basin in the west. This region underwent not only the evolution of the Paleo-Asian oceanic tectonic system in the Paleozoic, but was later overprinted and modified in the Mesozoic– Cenozoic by events related to the circum-Pacific tectonic system. Zhangguangcai Range are characterized by voluminous Phanerozoic granitoids, with rare Paleozoic strata and late Mesozoic volcanic and sedimentary strata occurring as remnants in a ‘‘sea’’ of granitoids (Wu et al., 2000, 2002).