黑龙江省东部早古生代地层的确定：地质与碎屑锆石U-Pb年代学证据

高福红; 杨扬; 王枫; 许文良

doi:10.3799/dqkx.2014.048

Volume 39 Issue 5

May 2014

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Article Navigation > Earth Science > 2014 > 39(5): 499-508

Gao Fuhong, Yang Yang, Wang Feng, Xu Wenliang, 2014. Determination of the Early Paleozoic Strata in Eastern Heilongjiang Province: Evidence from Field Geology and Detrital Zircon U-Pb Geochronology. Earth Science, 39(5): 499-508. doi: 10.3799/dqkx.2014.048

Citation:

Gao Fuhong, Yang Yang, Wang Feng, Xu Wenliang, 2014. Determination of the Early Paleozoic Strata in Eastern Heilongjiang Province: Evidence from Field Geology and Detrital Zircon U-Pb Geochronology. Earth Science, 39(5): 499-508. doi: 10.3799/dqkx.2014.048

Citation:

Gao Fuhong, Yang Yang, Wang Feng, Xu Wenliang, 2014. Determination of the Early Paleozoic Strata in Eastern Heilongjiang Province: Evidence from Field Geology and Detrital Zircon U-Pb Geochronology. Earth Science, 39(5): 499-508. doi: 10.3799/dqkx.2014.048

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Determination of the Early Paleozoic Strata in Eastern Heilongjiang Province: Evidence from Field Geology and Detrital Zircon U-Pb Geochronology

doi: 10.3799/dqkx.2014.048

College of Earth Sciences, Jilin University, Changchun 130061, China

Received Date: 2013-11-19
Publish Date: 2014-05-01

Abstract

Abstract

This paper reports LA-ICP-MS zircon U-Pb dating results from the Chenming and Baoquan formations in the eastern Heilongjiang Province in order to constrain their forming age and provenances. Most of detrital zircons are euhedral-subhedral in shape and display striped absorption or oscillatory zoning in CL images, implying their magmatic origin. The others show dark accretionary rim formed by metamorphism. The dating results on magmatic zircons indicate that 59 detrital zircons from feldspathic quartz sandstones in the upper part of the Chenming Formation yielded age populations of 561 Ma, 621 Ma, 683 Ma, 752 Ma, 803 Ma, 822 Ma, 851 Ma, 900 Ma, 922 Ma, 954 Ma, 1 781 Ma, 1 865 Ma and 1 933 Ma. Based on detrital zircon dating results, we conclude that the sedimentary processes of the Chenming Formation could take place after 561 Ma. In the study area, the Baoquan Formation overlain the Chenming Formation with the unconformity relationship, 60 detrital zircons from argillic slates in the lower part of the Baoquan Formation yielded age populations of 425 Ma, 450 Ma, 485 Ma, 900 Ma and 1 750 Ma. According to the above dating results and the field geological relationship, combined with the age populations of the detrial zircons from the Late Paleozoic strata, we consider that the Chenming Formation in the eastern Heilongjiang Province formed between 561 Ma to 510 Ma. The Early Paleozoic strata are firstly discovered with the exact geochronological evidence in the eastern Heilongjiang Province. The above detrital zircon ages indicate that the provenances of the Chenming Formation could mainly come from the Neoproterozoic and Paleoproterozoic igneous rocks around the study area, implying that the minor Precambrian basement relic might be occurred in the eastern margin of the Songnen-Zhangguangcailing Massif in the Early Paleozoic.
- eastern Heilongjiang Province,
- Early Paleozoic,
- Chenming Formation,
- detrital zircon U-Pb,
- geochronology,
- geology

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References(34)

References

Anderson, T., 2002. Correction of Common Lead in U-Pb Analyses that do not Report ²⁰⁴Pb. Chemical Geology, 192: 59-79. doi: 10.1016/S0009-2541(02)00195-X

Bruguier, O., Lancelet, J.R., 1997. U-Pb Dating on Single Detrital Zircon Grains from the Triassic Songpan-Ganze Flysch (Central China): Provenance and Tectonic Correlations. Earth and Planetary Science Letters, 152: 217-231. doi: 10.1016/S0012-821X(97)00138-6

Feng, J., 2012. Tectonic Properties of Yichun-Yanshou Tectonic Zone during Early Paleozoic(Dissertation). Jinlin University, Changchun (in Chinese with English abstract).

Han, G.Q., Liu, Y.J., Neubauer, F., et al., 2011. Origin of Terranes in the Eastern Central Asian Orogenic Belt, NE China: U-Pb Ages of Detrital Zircons from Ordovician-Devonian Sandstones, North Da Xing'an Mts. Tectonophysics, 511(3-4): 109-124. doi: 10.1016/j.tecto.2011.09.002

Heilongjiang Bureau of Geology and Mineral Resources, 1993. Regional Geology of Heilongjiang Province. Geological Publishing House, Beijing(in Chinese).

Li, J.Y., 2006. Peimian Geodynamic Setting of Northeast China and Adjacent Regions: Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate. Journal of Asian Earth Sciences, 26: 207-224. doi: 10.1016/j.jseaes.2005.09.001

Li, J.Y., Zhang, J., Yang, T.N., et al., 2009. Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Iis Adjacent Areas. Journal of Jilin University (Earth Science Edition), 39(4): 584-605(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200904002.htm

Li, W.M., Akira, T., Liu, Y.J., et al., 2009. ⁴⁰Ar/³⁹Ar Ages of the High-P/T Metamorphic Rocks of the Heilongjiang Complex in the Jiamusi Massif, Northeastern China. Journal of Mineralogical and Petrological Sciences, 104: 110-116. doi: 10.2465/jmps.081022g

Liu, Y.S., Gao, S., Hu, Z.C., et al., 2010. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen: U-Pb Dating, Hf Isotopes and Trace Elements in Zircons of Mantle Xenoliths. Journal of Petrology, 51: 537-571. doi: 10.1093/petrology/egp082

Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008. In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard. Chemical Geology, 257: 34-43. doi: 10.1016/j.chemgeo.2008.08.004

Lü, Z.C., Duan, G.Z., Hao, L.B., et al., 2001. Magmatism and Its Tectonic Significance in the Manzhouli-E'ergona Region. J. Mineral. Petrol. , 21(1): 77-85(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS200101016.htm

Lü, Z.C., Duan, G.Z., Hao, L.B., et al., 2002. Geochemistry and Tectonic Setting of Metamorphic Detrital Rock of Jiageda Group. Journal of Jilin University (Earth Science Edition), 32(2): 111-115(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CCDZ200202001.htm

Ludwig, K.R., 2003. ISOPLOT 3: A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Centre Special Publication, Berkeley, 74.

Miao, L.C., Liu, D.Y., Zhang, F.Q., et al., 2007. Zircon SHRIMP U-Pb Ages of the "Xinghuadukou Group" in Hanjiayuanzi and Xinlin Areas and the "Zhalantun Group" in Inner Mongolia, Da Hinggan Mountains. Chinese Science Bulletin, 52: 1112-1134. Doi: 10.1007/s11434-007-0131-2

Miao, L.C., Qiu, Y.M., McNaughton, N.J., et al., 2003. SHRIMP U-Pb Zircon Ages of Granitoids in the Wulashan Gold Deposit, Inner Mongolia, China: Timing of Mineralization and Tectonic Implications. International Geology Review, 45: 548-562. doi: 10.2747/0020-6814.45.6.548

Meng, E., Xu, W.L., Pei, F.P., et al., 2010. Detrital-Zircon Geochronology of Late Paleozoic Sedimentary Rocks in Eastern Heilongjiang Province, NE China: Implications for the Tectonic Evolution of the Eastern Segment of the Central Asian Orogenic Belt. Tectonophysics, 53: 1231-1245. doi: 10.1016/j.tecto.2009.11.015

Sengör, A.M.C., Natal'in, B.A., Burtman, V.S., 1993. Evolution of the Altaid Tectonic Collage and Paleozoic Crustal Growth in Eurasia. Nature, 364: 299-307. doi: 10.1038/364299a0

Tang, J., Xu, W.L., Wang, F., et al., 2013. Geochronology and Geochemistry of Neoproterozoic magmatism in the Erguna Massif, NE China: Petrogenesis and Implications for the Breakup of the Rodinia Supercontinent. Precambrian Research, 224: 597-611. doi: 10.1016/j.precamres.2012.10.019

Wang, F., Xu, W.L., Meng, E., et al., 2012a. Early Paleozoic Amalgamation of the Songnen-Zhangguangcai Range and Jiamusi Massifs in the Eastern Segment of the Central Asian Orogenic Belt: Geochronological and Geochemical Evidence from Granitoids and Rhyolites. Journal of Asian Earth Sciences, 49: 234-248. doi: 10.1016/j.jseaes.2011.09.022

Wang, F., Xu, W.L., Gao, F.H., et al., 2012b. Tectonic History of the Zhangguangcailing Group in Eastern Heilongjiang Province, NE China: Constraints from U-Pb Geochronology of Detrital and Magmatic Zircons. Tectonophysics, 566-567: 105-122. doi: 10.1016/j.tecto.2012.07.018

Wang, F., Xu, W.L., Gao, F.H., et al., 2013. Precambrian Terrane within the Songnen-Zhangguangcai Range Massif, NE China: Evidence from U-Pb Ages of Detrital Zircons from the Dongfengshan and Tadong Groups. Gondwana Research, 6: 1-12. doi: org/10.1016/j.gr.2013.06.017

Wilde, S.A., Wu, F.Y., Zhang, X.Z., 2003. Late Pan-African Magmatism in Northeast China: U-Pb SHRIMP Zircon Evidence for Igneous Ages from the Mashan Complex. Precambrian Res. , 122: 311-327. doi: 10.1016/S0301-9268(02)00217-6

Wilde, S.A., Zhang, X.Z., Wu, F.Y., 2000. Extension of a Newly-Identified 500 Ma Metamorphic Terrain in Northeast China: Furthur U-Pb SHRIMP Dating of Mashan Complex, Heilongjiang Province, China. Tectonophysics. , 328: 115-130. doi: 10.1016/S0040-1951(00)00180-3

Wu, F.Y., Sun, D.Y., Ge, W.C., et al., 2011. Geochronology of the Phanerozoic Granitoids in Northeastern China. Journal of Asian Earth Sciences, 41: 1-30. doi: 10.1016/j.jseaes.2010.11.014

Xu, M.J., Xu, W.L., Wang, F., et al., 2012. Age, Association and Provenance of the "Neoproterozoic" Fengshuigouhe Group in the Northwestern Lesser Xing'an Range, NE China: Constraints from Zircon U-Pb Geochronology. Journal of Earth Science, 23: 786-801. doi: 10.1007/s12583-012-0291-0

Yu, J.J., Wang, F., Xu, W.L., et al., 2013. Late Permian Tectonic Evolution at the Southeastern Margin of the Songnen-Zhangguangcai Range Massif, NE China: Constraints from Geochronology and Geochemistry of Granitoids. Gondwana Research, 24: 635-647. doi: 10.1016/j.gr.2012.11.015

Yuan, H.L., Gao, S., Liu, X.M., et al., 2004. Accurate U-Pb Age and Trace Element Determinations of Zircon by Laser Ablation Inductively Coupled Plasma Mass Spectrometry. Geostandard Newsletter, 28: 353-370. doi: 10.1111/j.1751-908X.2004.tb00755.x

Zhou, J.B., Simon, A., Wilde, S.A., et al., 2011. A > 1 300 km Late Pan-African Metamorphic Belt in NE China: New Evidence from the Xing'an Block and Its Tectonic Implications. Tectonophysics, 509: 280-292. doi: 10.1016/j.tecto.2011.06.018

Zhou, J.B., Wilde, S.A., Zhang, X.Z., et al., 2009. The Onset of Pacific Margin Accretion in NE China: Evidence from the Heilongjiang High-Pressure Metamorphic Belt. Tectonophysics, 478: 230-246. doi: 10.1016/j.tecto.2009.08.009

冯坚, 2012. 伊春-延寿构造带早古生代构造属性研究(硕士学位论文). 长春: 吉林大学.

黑龙江省地质矿产局, 1993. 黑龙江省区域地质志. 北京: 地质出版社.

李锦轶, 张进, 杨天南, 等, 2009. 北亚造山区南部及其毗邻地区地壳构造分区与构造演化. 吉林大学学报(地球科学版), 39(4): 584-605. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200904002.htm

吕志成, 段国正, 郝立波, 等, 2001. 满洲里—额尔古纳地区岩浆作用及其大地构造意义. 矿物岩石, 21(1): 77-85. doi: 10.3969/j.issn.1001-6872.2001.01.017

吕志成, 段国正, 郝立波, 等, 2002. 佳疙瘩组变碎屑岩地球化学特征及古构造环境. 吉林大学学报(地球科学版), 32(2): 111-115. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200202001.htm

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