扬子陆核北崆岭地区“马槽园群”的新认识
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摘要
扬子陆核北崆岭地区孔子河-樟村坪一带的"马槽园群"被认为是崆岭地区唯一出露的青白口纪沉积记录,对探讨扬子陆块在Rodinia超大陆中的位置及汇聚与裂解过程具有重要意义.通过对其进行岩石学、沉积学和碎屑锆石年代学研究,并与紧密伴存的南沱组进行对比,结果表明:"马槽园群"与南沱组的空间分布、砾石大小、分选、磨圆等特征相似,都体现了快速混杂堆积特点;最年轻锆石年龄限定"马槽园群"沉积时代晚于786Ma,南沱组则在657~635Ma之间,两者具有相似的碎屑锆石年龄谱特征.由此表明北崆岭地区的这套杂砾岩为新元古代冰碛岩,可与区域上南沱组对比,同属Marinoan冰期产物,而不能以马槽园群称之;其沉积物源来自于邻近崆岭杂岩、黄陵花岗岩和神农架群.
The "Macaoyuan Group"in Kongzihe-Zhangcunping area,regarded as the sole sediment of Qingbaikou Period in North Kongling area,plays an important role to understanding the convergence and cracking of Rodinia Supercontinent.Here,new petrology,sedimentology,and detrital zircon chronology studies are conducted on 12 sections in Kongzihe-Zhangcunping area.The"Macaoyuan Group"is similar with the Nantuo Formation in the distribution and gravel features.The U-Pb ages of detridal zircon indicate the"Macaoyuan Group"is younger than 786 Ma,and the Nantuo Formation is constrained between657 Ma and 635 Ma.The new findings indicate that the diamictite of"Macaoyuan Group"in North Kongling area is Neoproterozoic tillite,most likely time-equivalent to the Nantuo Formation.The sediment provenance is from the Kongling Group,Shennongjia Group and Huangling granite.
The "Macaoyuan Group"in Kongzihe-Zhangcunping area,regarded as the sole sediment of Qingbaikou Period in North Kongling area,plays an important role to understanding the convergence and cracking of Rodinia Supercontinent.Here,new petrology,sedimentology,and detrital zircon chronology studies are conducted on 12 sections in Kongzihe-Zhangcunping area.The"Macaoyuan Group"is similar with the Nantuo Formation in the distribution and gravel features.The U-Pb ages of detridal zircon indicate the"Macaoyuan Group"is younger than 786 Ma,and the Nantuo Formation is constrained between657 Ma and 635 Ma.The new findings indicate that the diamictite of"Macaoyuan Group"in North Kongling area is Neoproterozoic tillite,most likely time-equivalent to the Nantuo Formation.The sediment provenance is from the Kongling Group,Shennongjia Group and Huangling granite.
引文
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Han,P.Y.,Guo,J.L.,Chen,K.,et al.,2017.Widespread Neoarchean(~2.7-2.6Ga)Magmatism of the Yangtze Craton,South China,as Revealed by Modern River Detrital Zircons.Gondwana Research,42:1-12.https://doi.org/10.1016/j.gr.2016.09.006
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Liu,P.J.,Li,X.H.,Chen,S.M.,et al.,2015.New SIMS U-Pb Zircon Age and Its Constraint on the Beginning of the Nantuo Glaciation.Chinese Science Bulletin,60(10):958-963.https://doi.org/10.1007/s11434-015-0790-3
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Peng,S.B.,Kusky,T.M.,Jiang,X.F.,et al.,2012.Geology,Geochemistry,and Geochronology of the Miaowan Ophiolite,Yangtze Craton:Implications for South Chinas Amalgamation History with the Rodinian Supercontinent.Gondwana Research,21(2-3):577-594.https://doi.org/10.1016/j.gr.2011.07.010
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Wei,J.Q.,Wang,J.X.,2012.Zircon Age and Hf Isotope Compositions of Amphibolite Enclaves from the Kongling Complex.Geological Journal of China Universities,18(4):589-600.
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Chen,K.,Gao,S.,Wu,Y.B.,et al.,2013.2.6-2.7Ga Crustal Growth in Yangtze Craton,South China.Precambrian Research,224:472-490.https://doi.org/10.1016/j.precamres.2012.10.017
Condon,D.,Zhu,M.,Bowring,S.,et al.,2005.U-Pb Ages from the Neoproterozoic Doushantuo Formation,China.Science,308(5718):95-98.https://doi.org/10.1126/science.1107765
Deng,Q.,Wang,J.,Wang,Z.J.,2013.New Evidence for the Age of the Macaoyuan Group on the Northern Margin of the Yangtze Block,South China-Implications for Stratigraphic Correlation and Palaeogeographic Framework.Geological Bulletin of China,32(4):631-638(in Chinese with English abstract).
Gao,S.,Yang,J.,Zhou,L.,et al.,2011.Age and Growth of the Archean Kongling Terrain,South China,with Emphasis on3.3Ga Granitoid Gneisses.American Journal of Science,311(2):153-182.https://doi.org/10.2475/02.2011.03
Gao,W.,Zhang,C.H.,2009.Zircon SHRIMP U-Pb Ages of the Hnangling Granite and the Tuff Beds from Liantuo Formation in the Three Gorges Area of Yangtze River,China and Its Geological Significance.Geological Bulletin of China,28(1):45-50(in Chinese with English abstract).
Guo,J.L.,Wu,Y.B.,Gao,S.,et al.,2015.Episodic PaleoarcheanPaleoproterozoic(3.3-2.0Ga)Granitoid Magmatism in Yangtze Craton,South China:Implications for Late Archean Tectonics.Precambrian Research,270:246-266.https://doi.org/10.1016/j.precamres.2015.09.007
Han,P.Y.,Guo,J.L.,Chen,K.,et al.,2017.Widespread Neoarchean(~2.7-2.6Ga)Magmatism of the Yangtze Craton,South China,as Revealed by Modern River Detrital Zircons.Gondwana Research,42:1-12.https://doi.org/10.1016/j.gr.2016.09.006
Hu,R.,Li,S.Q.,Wang,W.,2016.Source Characteristics of Tillite the Nantuo Formation in Three Gorges,Northern Yangtze Block:Evidences from Zircon Ages and Geochemical Composition.Earth Science,41(10):1630-1654(in Chinese with English abstrat).https://doi.org/10.3799/dqkx.2016.121
Hu,Z.X.,Liu,Z.X.,Zhang,Y.L.,2012.Determination of the Bottom Boundary of Shennongjia Gr in Pre-Nanhuan Period about the Northern Margin of Yantze Massif and Its Geological Significance.Resources Environment and Engineering,26(3):201-208(in Chinese with English abstract).
Hubei Geological Bureau,1990.Regional Geology of Hubei Province.Geological Publishing House,Beijing,5-43(in Chinese).
Jiao,W.F.,Wu,Y.B.,Yang,S.H.,et al.,2009.The Oldest Basement Rock in the Yangtze Craton Revealed by Zircon U-Pb Age and Hf Isotope Composition.Science China Earth Sciences,52(9):1393-1399.https://doi.org/10.1007/s11430-009-0135-7
Li,H.K.,Zhang,C.L.,Xiang,Z.Q.,et al.,2013.Zircon and Baddeleyite U-Pb Geochronology of the Shennongjia Group in the Yangtze Craton and Its Tectonic Significance.Acta Petrologica Sinica,29(2):673-697(in Chinese with English abstract).
Li,Q.,Leng,J.,1987.The Upper Precambrian in the Shennongjia Region.Tianjin Science and Technology Publishing House,Tianjin(in Chinese).
Li,Y.H.,Zheng,J.P.,Xiong,Q.,et al.,2016.Petrogenesis and Tectonic Implications of Paleoproterozoic Metapelitic Rocks in the Archean Kongling Complex from the Northern Yangtze Craton,South China.PrecambrianResearch,276:158-177.https://doi.org/10.1016/j.precamres.2016.01.028
Liu,C.X.,Mao,X.W.,Wei,Y.X.,et al.,2004.A Preliminary Research on Stratigraphic Sequence of Shennongjia Group.Resources Environment&Engineering,18(Z1):5-16(in Chinese with English abstract).
Liu,P.J.,Li,X.H.,Chen,S.M.,et al.,2015.New SIMS U-Pb Zircon Age and Its Constraint on the Beginning of the Nantuo Glaciation.Chinese Science Bulletin,60(10):958-963.https://doi.org/10.1007/s11434-015-0790-3
Ma,G.G.,Li,H.Q.,Zhang,Z.C.,1984.An Investigation of the Age Limits of the Sinian System in South China.Bulletin of Yichang Institute Geology and Mineral Resources of Chinese Academy of Geological Sciences,8:1-29(in Chinese with English abstract).
Peng,S.B.,Han,Q.S.,Ali,P.,et al.,2016.Discovery of the Paleproterozoic Ophio1itic Melange in the North Part of Huangling Dome,Yangtze Craton.Earth Science,41(12):2117-2118.
Peng,S.B.,Kusky,T.M.,Jiang,X.F.,et al.,2012.Geology,Geochemistry,and Geochronology of the Miaowan Ophiolite,Yangtze Craton:Implications for South Chinas Amalgamation History with the Rodinian Supercontinent.Gondwana Research,21(2-3):577-594.https://doi.org/10.1016/j.gr.2011.07.010
Qiu,X.F.,Ling,W.L.,Liu,X.M.,et al.,2011.Recognition of Grenvillian Volcanic Suite in the Shennongjia Region and Its Tectonic Significance for the South China Craton.Precambrian Research,191(3-4):101-119.https://doi.org/10.1016/j.precamres.2011.09.011
Qiu,X.F.,Yang,H.M.,Zhang,L.G.,et al.,2015.Geochronology of Serpentinized Harzburgite in Miaowan Ophiolite,Yangtze Block and Its Tectonic Implications.Earth Science,40(7):1121-1128(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2015.094
Qiu,Y.M.,Gao,S.,McNaughton,N.J.,et al.,2 000.First Evidence of>3.2Ga Continental Crust in the Yangtze Craton of South China and Its Implications for Archean Crustal Evolution and Phanerozoic Tectonics.Geology,28(1):11-14.https://doi.org/10.1130/0091-7613(2000)028<0011:feogcc>2.3.co;2
Qiu,Y.S.,Hu,Z.X.,Yang,Q.X.,et al.,2013.LA-ICP-MS U-Pb Dating for the Macaoyuan Group in South China and Its Stratigraphic Significance.Resources Environment and Engineering,27(3):328-334(in Chinese with English abstract).
Wang,J.,Deng,Q.,Wang,ZJ..,et al.,2013.New Evidences for Sedimentary Attributes and Timing of the“Macaoyuan Conglomerates”on the Northern Margin of the Yangtze Block inSouthern China.Precambrian Research,235:58-70.https://doi.org/10.1016/j.precamres.2013.06.003
Wang,ZJ..,Huang,Z.G.,Yao,J.X.,et al.,2014.Characteristics and Main Progress of the Stratigraphic Chart of China and Directions.Acta Geoscientica Sinica,35(3):271-276.
Wei,J.Q.,Wang,J.X.,2012.Zircon Age and Hf Isotope Compositions of Amphibolite Enclaves from the Kongling Complex.Geological Journal of China Universities,18(4):589-600.
Wei,Y.X.,Peng,S.B.,Jiang,X.F.,et al.,2012.SHRIMP Zircon U-Pb Ages and Geochemical Characteristics of the Neoproterozoic Granitoids in the Huangling Anticline and Its Tectonic Setting.Journal of Earth Science,23(5):659-676.https://doi.org/10.1007/s12583-012-0284-z
Xiong,C.Y.,Wei,C.S.,Jin,G.F.,et al.,2004.Pre-Sinian Paleostructural Framework and Major Geological Events in the Huangling Anticline,western Hubei.Journal of Geomechanics,10(2):97-112(in Chinese with English abstract).
Xu,D.L.,Liu,H.,Wei,Y.X.,et al.,2016.Detrial Zircon U-Pb Dating of Zhengjiaya Formation from the Shennongjia Area in the Northern Yangtze Block and Its Tectonic Implications.Acta Geologica Sinica,90(10):2648-2660(in Chinese with English abstrat).
Ye,Q.,Tong,J.N.,Xiao,S.H.,et al.,2015.The Survival of Benthic Macroscopic Phototrophs on a Neoproterozoic Snowball Earth.Geology,43(6):507-510.https://doi.org/10.1130/g36640.1
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