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| Keywords | |
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Jiamusi--Mongolia block |
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continental margin deposit |
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Late Paleozoic strata |
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northeastern China |
| Authors | |
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LI Ning-1 |
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WANG Cheng-Wen-1 |
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3 |
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SUN Yue-Wu-2 |
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3 |
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MA Xiao-Qin-1 |
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LIU Hui-1 |
| PubMed | |
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Article by Li, N. 1 |
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Article by Wang, C. W. 1 |
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Article by 3 |
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Article by Sun, Y. W. 2 |
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Article by 3 |
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Article by Ma, X. Q. 1 |
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Article by Liu, H. 1 |
Confirmation of Late Paleozoic marine strata belonging to continental margin deposit in northeastern China
LI Ning-1, WANG Cheng-Wen-1, 3, SUN Yue-Wu-2, 3, MA Xiao-Qin-1, LIU Hui-1
1�� College of Earth Sciences��Jilin University��Changchun 130061��China; 2�� Research Center of Paleontology �� Stratigraphy��Jilin University��Changchun 130026��China; 3�� Key-Lab for Evolution of Past Life and Environment in NE Asia��Ministry of Education��Jilin University�� Changchun 130026��China
The Late Paleozoic marine strata in northeastern China are distributed in zonal pattern and surrounding the Jiamusi--Mongolia block�� The unsteady sedimentation such as well-developed lithic feldspar sandstone�� transverse lithological variation��unstable lithofacies and development of volcanic rocks��indicated these strata belonging to active sediment�� From the core to the marginal suture belt of the Jiamusi --Mongolia block��obvious lithofacies change of old land --para --epicontinental sea --continental shelf sea --abyssal sea can be seen�� The authors suggested that the Late Paleozoic marine strata might belong to continental marginal deposits of Jiamusi --Mongolia block in northeastern China��based on the zonal distributions��active deposition��and regular distribution of the tectonic lithological zones��