Global Geology 2014, 17(4) 206-211 DOI:     ISSN: 1673-9736 CN: 22-1371/P

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Keywords
Tangjiatun Formation
trace elements
rare earth elements
sedimentary environment
Acheng
Heilongjiang
Authors
WANG Fukui
WU Jianan
LV Shicong
ZHAO Dalin
QU Xiyu and WANG Dehai
PubMed
Article by Wang F
Article by Wu J
Article by Lv S
Article by Zhao D
Article by Qu XAWD

Sedimentary environment of Late Carboniferous Tangjiatun Formation in Acheng of Heilongjiang

WANG Fukui, WU Jianan, LV Shicong, ZHAO Dalin, QU Xiyu and WANG Dehai

1. College of Earth Sciences,Jilin University,Changchun 130061,China; 2. Bohai Research Institute of Oilfield Exploration & Development,Tianjin Branch of CNOOC,Tianjin 300452,China; 3. School of Geosciences,China University of Petroleum (East China),Qingdao 266580,Shandong,China

Abstract

According to the lithological assemblages and elemental geochemistry of the measured profile,the authors studied the sedimentary and tectonic environment of the Late Carboniferous Tangjiatun Formation in Acheng. The results show that the trace elements of mudstone samples from Tangjiatun Formation have the char- acteristics of high Th,V and Cu,but low Ba,Nb and Sr. The rare earth elements are characterized by signifi- cantly light and heavy rare earth elements differentiation,relative enrichment of light rare earth elements,and a negative anomaly of δEu. The Tangjiatun Formation belongs to a marine and delta sedimentary environment, and its tectonic setting is considered as a continental island arc environment.

Keywords Tangjiatun Formation   trace elements   rare earth elements   sedimentary environment   Acheng   Heilongjiang  
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