Geochemistry, Geochronology, and Hf isotopic Composition of the Late Paleoproterozoic Lujiapuzi Formation, NE Yan-Liao Rift, Northern Liaoning
Jin LIU
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Search for more papers by this authorCorresponding Author
Jian ZHANG
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Corresponding author. E-mail: [email protected]Search for more papers by this authorZhenghong LIU
College of Earth Sciences, Jilin University, Changchun 130061 Jilin, China
Search for more papers by this authorChangqing YIN
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Search for more papers by this authorChen ZHAO
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Search for more papers by this authorYoubo PENG
Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031 Liaoning, China
Search for more papers by this authorShiyong DOU
Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031 Liaoning, China
Search for more papers by this authorZhongjie YANG
Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031 Liaoning, China
Search for more papers by this authorJin LIU
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Search for more papers by this authorCorresponding Author
Jian ZHANG
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Corresponding author. E-mail: [email protected]Search for more papers by this authorZhenghong LIU
College of Earth Sciences, Jilin University, Changchun 130061 Jilin, China
Search for more papers by this authorChangqing YIN
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Search for more papers by this authorChen ZHAO
School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510275 Guangdong, China
Guangdong Provincal Key Lab of Geodynamics and Geohazards, School of Earth Sciences and Engineering, Sun Yat-sen University, Guangzhou 510372 Guangdong, China
Search for more papers by this authorYoubo PENG
Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031 Liaoning, China
Search for more papers by this authorShiyong DOU
Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031 Liaoning, China
Search for more papers by this authorZhongjie YANG
Liaoning Survey Academy of Geology and Mineral Resources, Shenyang 110031 Liaoning, China
Search for more papers by this authorAbout the first author: LIU Jin, male; born in 1986 in Chongqing City; postdoctoral fellow of School of Earth Sciences and Engineering, Sun Yat-sen University. He is now work on regional geological survey and interested in the study on evolution of the North China Craton. Email: [email protected]; phone: 15942039295.
Abstract
The metasedimentary Lujiapuzi Formation crops out along the northeastern margin of the North China Craton, close to the Yan-Liao Rift. The age and tectonic setting of the formation, and its relationship with the Yan-Liao Rift are currently unclear. Here we present detrital zircon U-Pb ages, and Hf isotopic and geochemical data for the Lujiapuzi Formation to constrain the timing of deposition, the provenance of the formation, and the regional stratigraphy relationship. Zircon U-Pb dating constrains the timing of deposition of the Lujiapuzi Formation to younger than 1780 Ma, and indicates that most grains were sourced from the Longgang Block and the Paleoproterozoic Liao-Ji Belt. Detailed field investigations and a correlation of the regional stratigraphy reveal that much of the Lujiapuzi Formation is equivalent to the Tuanshanzi Formation in the Yan-Liao Rift; the lower section may represent the earliest sediments deposited within the Fanhe Basin. Based on these results and the findings of previous studies, we suggest that the base of the Changcheng System has an age of 1.80 Ga. Zircon Hf isotopic data indicate that the main period of crustal growth along the northeastern margin of the North China Craton occurred at 3.2–2.5 Ga, with a peak at 2.9–2.7 Ga.
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