Biostratigraphy and Geometric Morphometrics of Conchostracans from the Middle Triassic in Southern Lancangjiang Zone
-
摘要: 三叠纪火山-沉积岩是南澜沧江带的重要组成部分，长期缺乏可靠的生物地层学研究.首次报道了该地区忙怀组叶肢介化石，包括3个种和1个未定种：Euestheria minuta、Euestheria yipinglangensis、Euestheria dazuensis和Euestheria sp..对保存较好的叶肢介个体进行了8个特征参数的测量，并对叶肢介化石进行了定量和半定量描述.将获得的壳体长度和宽度进行压轴回归（RMA）线性拟合，发现二者具有明显的线性相关性.简单线性测量数据主成分分析和壳体轮廓傅里叶系数主成分分析结果均表明，E.minuta、E. sp.、E.yipinglangensis和E.dazuensis有较大程度的种内变化.结合化石组合和同位素测年结果，认为南澜沧江带忙怀组上部时代已延伸至中三叠世拉丁期.Abstract: The Triassic volcanic and sedimentary rocks are the important components in the geological records of the southern Lancangjiang zone.However, little is known about the biostratigraphic correlation in this area.In this study, three species and one indeterminate species in one genera of conchostracans were recognized for the first time from the Manghuai Formation of the study area, including Euestheria minuta, Euestheria yipinglangensis, Euestheria dazuensis and Euestheria sp..For the purpose of the comparison, quantitative and semi-quantitative descriptions of the specimens, we took eight standard linear measurements from each well-preserved specimen.A reduced major axis (RMA) regression line has been fitted to the scatter of carapace length versus carapace height, showing a significant linear correlation between them.In addition, the principal component analysis of the linear measurements and fourier coefficients for the outlines of the conchostracan specimens indicates a great deal of intraspecific variations among these four species.Finally, it is suggested that the upper part of the Manghuai Formation in the southern Lancangjiang zone is the Middle Triassic (Ladinian) depositions according to the fossils assemblage and isotopic dating evidences.
-
图 1 南澜沧江带区域地质简图
图a为南澜沧江带三叠纪岩浆岩分布，据Wang et al.(2010)修改；图b为研究区地质简图及剖面位置；图c为陶家村剖面柱状图.图a中231±5 Ma年龄据彭头平等(2006)；230.8±2.8 Ma年龄据韦诚等(2016)；236.7±2.2 Ma年龄据王硕等(2012)；248.5±6.3 Ma年龄据Peng et al.(2008)；230±2 Ma年龄据Peng et al.(2013).1.泥岩；2.粉砂质板岩；3.粉砂岩；4.砂岩；5.含砾砂岩；6.砂质砾岩；7.砾岩；8.英安岩；9.火山角砾岩；10.凝灰岩；11.玄武岩；12.同位素年龄；13.叶肢介化石；14.植物化石；15.水平层里；16.平行层理；17.雨痕；18.正粒序层理
Fig. 1. Simplified geological map for the southern Lancangjiang zone
图 2 叶肢介化石线性数据测量示意图
据Scholze and Schneider (2015)，Hethke et al.(2016)修改.L.标本的总长，取最前缘和最后缘点之间的直线距离；H.高度，是腹缘最下部点到背缘前后端点水平连线之间的垂直距离；arr.背缘最后端点到后缘最大弯曲点的切线的垂直距离；av.背缘前端点到前缘切线的垂直距离；a.壳体前缘最大弯曲点到背缘前后端点水平连线间的直线距离；b.壳体后缘最大弯曲点到背缘前后端点水平连线间的直线距离；c.腹缘最大弯曲点到前缘最大弯曲点切线之间的垂直距离；Ch.背缘的长度
Fig. 2. The schematic diagram of linear data measurements of the conchostracans
图 3 叶肢介化石壳体长与高线性拟合图
图中x=lgH，y=lgL
Fig. 3. Linear fit map of length and width of conchostracans
图 4 壳体线性测量数据的主成分分析
Fig. 4. Principal components analysis of linear measurement data for the conchostracans
图 5 E. sp.、E.yipinglangensis和E.dazuensis轮廓傅里叶系数的主成分分析
Fig. 5. Principal components analysis of Fourier coefficients for carapace profile, comparison of the three groups (E.sp., E.yipinglangensis and E.dazuensis)
图 6 南澜沧江带中三叠统忙怀组Euestheria minuta(a~f)和英国的Euestheria minuta(g~p)
a.左瓣印模，标本号PM301-49-1；b.右瓣印模，标本号PM301-56-1；c.左瓣印模，标本号PM301-56-3；d.右瓣印模，标本号PM301-58-5；e.左瓣印模，标本号PM301-63-1；f.左瓣印模，标本号PM301-63-2；g~h.右瓣印模；i.左瓣印模；j~k.右瓣；l~m.左瓣；n.右瓣；o.右瓣外模；p.左瓣.图中比例尺均为1 mm
Fig. 6. Euestheria minuta from the Middle Triassic Manghuai Formation, southern Lanchangjiang zone (a-f) and United Kingdom (g-p)
图 7 南澜沧江带中三叠统忙怀组Euestheria dazuensis
a.右瓣，标本号PM301-1；b.左瓣，标本号PM301-3-2；c.左瓣，标本号PM301-18-3；d.左瓣外模，标本号PM301-39；e.右瓣外模，标本号PM301-36-1；f.右瓣，标本号PM301-3-3；g.左瓣，标本号PM301-7-1；h.左瓣，标本号PM301-14-3；i.左瓣，标本号PM301-10.图中比例尺均为1 mm
Fig. 7. Euestheria dazuensis from the Middle Triassic Manghuai Formation, southern Lanchangjiang zone
图 8 南澜沧江带中三叠统忙怀组Euestheria sp.
a.左瓣，标本号PM301-19；b.右瓣，标本号PM301-18-2；c.左瓣外模，标本号PM301-30；d.左瓣印模，标本号PM301-56-2；e.左瓣印模，标本号PM301-43；f.左瓣印模，标本号PM301-55；g.左瓣外模，标本号301-7-7；h.右瓣印模，标本号PM301-38-1；i.左瓣外模，标本号PM301-42-1.图中比例尺均为1 mm
Fig. 8. Euestheria sp.from the Middle Triassic Manghuai Formation, southern Lanchangjiang zone
图 9 南澜沧江带中三叠统忙怀组Euestheria yipinglangensis
a.右瓣，标本号PM301-14-1；b.左瓣印模，标本编号PM301-32；c.左瓣，标本号PM301-52；d.右瓣印模，标本号PM301-7-6；e.右瓣印模，标本号PM301-12；f.右瓣外模，标本号PM301-14-2；g.左瓣，标本号PM301-7-5；h.左瓣印模，标本号PM301-2-2；i.左瓣，标本号PM301-52.图中比例尺均为1 mm
Fig. 9. Euestheria yipinglangensis from the Middle Triassic Manghuai Formation, southern Lanchangjiang zone
表 1 南澜沧江带忙怀组叶肢介化石简单线性测量数据的平均值和标准差
Table 1. Mean and standard deviation for linear measurements of conchostracans from Manghuai Formation in the southern Lancangjiang zone
平均值 a b c arr av Ch H L H/L Ch/L av/a arr/b Euestheria sp. 1.57 2.09 3.24 2.45 1.39 2.65 3.91 6.48 0.61 0.41 0.88 1.17 Euestheria yipinglangensis 1.70 2.18 2.86 1.96 1.11 2.91 4.36 5.98 0.73 0.49 0.64 0.91 Euestheria dazuensis 1.53 2.06 3.40 2.04 0.90 3.46 4.09 6.40 0.64 0.54 0.58 1.02 Euestheria minuta 0.72 0.99 1.58 0.91 0.37 1.92 1.99 3.20 0.62 0.60 0.38 0.93 Euestheria minuta(英国) 0.69 0.90 1.48 0.78 0.38 1.54 1.79 2.70 0.66 0.57 0.43 0.88 标准差 a b c arr av Ch H L H/L Ch/L av/a arr/b Euestheria minuta 0.24 0.21 0.28 0.44 0.45 0.55 0.40 0.58 0.03 0.09 0.24 0.17 Euestheria sp. 0.47 0.39 0.34 0.46 0.39 0.62 0.68 0.80 0.05 0.10 0.13 0.16 Euestheria franconica 0.29 0.45 0.49 0.42 0.38 0.70 0.57 0.91 0.06 0.08 0.17 0.27 Euestheria minuta 0.17 0.14 0.21 0.26 0.09 0.38 0.24 0.41 0.07 0.08 0.09 0.23 Euestheria minuta(英国) 0.10 0.11 0.26 0.15 0.09 0.34 0.23 0.36 0.02 0.07 0.14 0.19 
下载: 导出CSV
-
Astrop, T.I., Sahni, V., Blackledge, T.A., et al., 2015.Mechanical Properties of the Chitin-Calcium-Phosphate "Clam Shrimp" Carapace (Branchiopoda:Spinicaudata):Implications for Taphonomy and Fossilization.Journal of Crustacean Biology, 35(2):123-131. https://doi.org/10.1163/1937240x-00002332 Chen, P.J., 2012.Cretaceous Conchostracan Biostratigraphy of China.Journal of stratigraphy, 36(2):300-313 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DCXZ201202013.htm Defretin-Lefranc, S., 1965.Étude et révision de Phyllopoda Conchostracés en provenance U.R.S.S.Annales de la Société Géologique du Nord, 85:15-48. Depéret, C., Mazeran, P., 1912.Les Estheria du Permien d'Autun.Société d'Histoire Naturalle d'Autun Bulletin, 25:165-173. http://www.researchgate.net/publication/309384389_Les_Estheria_du_Permien_d'Autun Dewey, J.F., Shackleton, R.M., Chang, C.F., et al., 1988.The Tectonic Evolution of the Tibetan Plateau.Philosophical Transactions of the Royal Society B Biological Sciences, 327(1594):379-413. doi: 10.1098/rsta.1988.0135 Dong, G.C., Mo, X.X., Zhao, Z.D., et al., 2013.Zircon U-Pb Dating and the Petrological and Geochemical Constraints on Lincang Granite in Western Yunnan, China:Implications for the Closure of the Paleo-Tethys Ocean.Journal of Asian Earth Sciences, 62:282-294. https://doi.org/10.1016/j.jseaes.2012.10.003 Fan, W.M., Peng, T.P., Wang, Y.J., 2009.Triassic Magmatism in the Southern Lancangjiang zone, Southwestern China and Its Constraints on the Tectonic Evolution of Paleo-Tethys.Earth Science Frontiers, 16(6):291-302 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy200906031 Gallego, O.F.1992.Conchostracos Triasicos de Mendoza y San Juan, Argentina.Ameghiniana, 29(2):159-175. http://www.mendeley.com/research/conchostracos-triasicos-mendoza-y-san-juan-argentina/ Gerstaecker, A., 1866. Crustacea (Erste Halfe). In: Bronn, H. G., ed., Die Klassen und Ordungen der Thier-Reichs, 5 (Part 1: Arthropoda). Akeademic Verlag, Leipzig. Hennig, D., Lehmann, B., Frei, D., et al., 2009.Early Permian Seafloor to Continental Arc Magmatism in the Eastern Paleo-Tethys:U-Pb Age and Nd-Sr Isotope Data from the Southern Lancangjiang Zone, Yunnan, China.Lithos, 113(3-4):408-422. https://doi.org/10.1016/j.lithos.2009.04.031 Hethke, M., Fürsich, F.T., Schneider, S., et al., 2016.Sex Determination of the Early Cretaceous Clam Shrimp Eosestheria Middendorfii (Yixian Formation, China).Lethaia, 50(1):105-121. https://doi.org/10.13039/501100002347 Jian, P., Liu, D.Y., Kröner, A., et al., 2009.Devonian to Permian Plate Tectonic Cycle of the Paleo-Tethys Orogen in Southwest China (Ⅱ):Insights from Zircon Ages of Ophiolites, Arc/Back-Arc Assemblages and within-Plate Igneous Rocks and Generation of the Emeishan CFB Province.Lithos, 113(3-4):767-784. https://doi.org/10.1016/j.lithos.2009.04.006 Jones, P.J., Chen, P.J., 2000.Carboniferous and Permian Leaioidea (Branchiopoda:Conchostraca) from Australia:Taxonomic Revision and Biostratigraphic Implications.Records of the Australian Museum, 52(2):223-244. https://doi.org/10.3853/j.0067-1975.52.2000.1315 Jones, T.R., 1863.On Fossil Estheriae andTheir Distribution.Quarterly Journal of the Geological Society, 19(1-2):140-157. https://doi.org/10.1144/gsl.jgs.1863.019.01-02.20 Kong, H.L., Dong, G.C., Mo, X.X., et al., 2012.Petrogenesis of Lincang Ganites in Sanjiang Area of Western Yunnan Province:Constraints from Geochemistry, Zircon U-Pb Geochronology and Hf Isotope.Acta Petrologica Sinica, 28(5):1438-1452 (in Chinese with English abstract). http://www.oalib.com/paper/1475010 Kozur, H.W., Weems, R.E., 2010.The Biostratigraphic Importance of Conchostracans in the Continental Triassic of the Northern Hemisphere.Geological Society, London, Special Publications, 334(1):315-417. https://doi.org/10.1144/sp334.13 Latreille, P. A., 1817. Le Re`gne Animal, Tome Ⅲ, Contenant les Crustaces, les Arachnides et les Insectes. A. Bedin, Paris. Leng, Q.F., Tang, J.X., Zheng, W.B., et al., 2016.Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet.Earth Science, 41(6):999-1015 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.083 Li, G., Chen, P.J., Wan, X.Q., et al., 2004.Stratotype of the Basal Boundary of the Nen Jiang Gian Stage, Cretaceous.Journal of stratigraphy, 28(4):297-299, 335 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ200404001.htm Li, X.L., 1996.Basic Characteristics and Formation Structural Environment of Lincang Composite Granite Batholith.Yunnan Geology, 15(1):1-18 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600616589 Liao, H.Y., Huang, D.Y., 2014.Jurassic Fossil Conchostracans from Bawanggou, Qinglong County, Hebei Frovince.Journal of Stratigraphy, 38(4):433-438 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DCXZ201404007.htm Linder, F., 1945.Affinities within the Branchiopoda with Notes on Some Dubious Fossils.Arkiv for Zoologi, 37A:1-28. http://ci.nii.ac.jp/naid/10007415993 Liu, C.S., Zhu, J.C., Xu, X.S., 1989.Study on the Characteristics of Lincang Composite Granite Batholith in West Yunnan.Yunnan Geology, 8(3-4):189-204 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YNZD1989Z1000.htm Luo, L., An, X.Y., Wu, N.W., et al., 2014.Evolution of Neoproterozoic-Mesozoic Sedimentary Basins in Bangong-Shuanghu-Nujiang-Changning-Menglian Suture Zone.Earth Science, 38(8):1169-1184 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-DQKX201408018.htm Martin, J.W., Davis, G.E., 2001.An Updated Classification of the Recent Crustacea.Natural History Museum of Los Angeles County Contributions in Science, 39:1-124. http://www.jstor.org/stable/1549650 Metcalfe, I., 2009.Late Palaeozoic and Mesozoic Tectonic and Palaeogeographical Evolution of SE Asia.Geological Society, London, Special Publications, 315(1):7-23. https://doi.org/10.1144/sp315.2 Morton, J.D., Whiteside, D.I., Hethke, M., et al., 2017.Biostratigraphy and Geometric Morphometrics of Conchostracans (Crustacea, Branchiopoda) from the Late Triassic Fissure Deposits of Cromhall Quarry, UK.Palaeontology, 60(3):349-374. https://doi.org/10.1111/pala.12288 Nanjing Institute of Geology and Palaeontology, Academia Sinica, 1974.A Brochure of Paleontology in the Southwest Region.Science Press, Beijing (in Chinese). Niu, S.W., Li, P.X., Cheng, Z.W., 2005.Upper Jurassic Conchostracan Fossils from Central Yunnan and Its Stratigraphic Significance.Geological Bulletin of China, 24(4):329-340 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/zgqydz200504006 Niu, S.W., Tian, S.G., Pang, Q.Q., 2010.Conchostracan Biostratigraphy of the Dadianzi Formation in the Luanping Basin, Northern Hebei, China and the Boundary of Continental Jurassic and Cretaceous Strata.Geological Bulletin of China, 29(7):961-979 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201007001 Peng, T.P., Wang, Y.J., Fan, W.M., et al., 2006.The SHRIMP Zircon U-Pb Dating of the Felsic Igneous Rocks from Southern Lancangjiang and Its Tectonic Implications.Science in China (Series D), 36(2):123-132 (in Chinese). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgkx-ed200610003 Peng, T.P., Wang, Y.J., Zhao, G.C., et al., 2008.Arc-Like Volcanic Rocks from the Southern Lancangjiang Zone, SW China:Geochronological and Geochemical Constraints on Their Petrogenesis and Tectonic Implications.Lithos, 102(1-2):358-373. https://doi.org/10.1016/j.lithos.2007.08.012 Peng, T.P., Wilde, S.A., Wang, Y.J., et al., 2013.Mid-Triassic Felsic Igneous Rocks from the Southern Lancangjiang Zone, SW China:Petrogenesis and Implications for the Evolution of Paleo-Tethys.Lithos, 168-169:15-32. https://doi.org/10.1016/j.lithos.2013.01.015 Rohlf, J. F. 2016. tpsDIG2w64, v. 2. 26. Department of Ecology & Evolution, State University of New York, Stony Brook. Schneider, J.W., Scholze, F., 2016.Late Pennsylvanian-Early Triassic Conchostracan Biostratigraphy:A Preliminary Approach.Geological Society, London, Special Publications, 450(1):365-386. https://doi.org/10.1144/sp450.6 Scholze, F., Schneider, J.W., 2015.Improved Methodology of 'Conchostracan' (Crustacea:Branchiopoda) Classification for Biostratigraphy.Newsletters on Stratigraphy, 48(3):287-298. https://doi.org/10.1127/nos/2015/0065 Şengör, A.M.C., Natal'in, B.A., Burtman, V.S., 1993.Evolution of the Altaid Tectonic Collage and Palaeozoic Crustal Growth in Eurasia.Nature, 364(6435):299-307. https://doi.org/10.1038/364299a0 Shen, Y., Gallego, O.F., Martínez, S., 2004.The Conchostracan Subgenus Orthestheria (Migransia) from the Tacua-Rembó Formation (Late Jurassic-Early Cretaceous, Uruguay) with Notes on Its Geological Age.Journal of South American Earth Sciences, 16:615-622. https://doi.org/10.1016/j.jsames.2003.02.001 Tasch, P., 1987. Fossil Conchostraca of the Southern Hemisphere and Continental Drift. Geological Society of America Memoir, 165. von Zieten, C. H., 1833. Die Versteinerungen Wurttembergs. Unsere Zeit, Stuttgart. Wang, E.Q., 2017.Timing of the Initial Collision between the Indian and Asian Continents.Science in China (Series D), 3(47):284-292 (in Chinese). http://kns.cnki.net/KCMS/detail/detail.aspx?filename=JDXG201704002&dbname=CJFD&dbcode=CJFQ Wang, S., Dong, G.C., Mo, X.X., et al., 2012.Petrological and Geochemical Characteristics, Ar-Ar Geochronology Study and Their Tectonic Significance of Triassic Volcanic Rocks in Southern Lancangjiang Zone.Acta Petrologica Sinica, 28(4):1148-1162 (in Chinese with English abstract). Wang, S.E., Li, G., 2008.New Fossil Clam Shrimps from the Tuchengzi Formation of Northern Hebei and Western Liaoning.Acta Palaeontologica Sinica, 47(3):319-325 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gswxb200803007 Wang, Y.J., Zhang, A.M., Fan, W.M., et al., 2010.Petrogenesis of Late Triassic Post-Collisional Basaltic Rocks of the Lancangjiang Tectonic Zone, Southwest China, and Tectonic Implications for the Evolution of the Eastern Paleotethys:Geochronological and Geochemical Constraints.Lithos, 120(3-4):529-546. https://doi.org/10.1016/j.lithos.2010.09.012 Wei, C., Qi, X.X., Chang, Y.L., et al., 2016.Identification on Age of Xiaodingxi Formation Volcanic Rocks in Central-Southern Lancangjiang Orogeny and Its Tectonic Implication.Acta Geologica Sinica, 90(11):3192-3214 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-DZXE201611014.htm Xi, D.P., Li G., Wan, X.Q., et al., 2009.Yaojia-Lower Nenjiang Formations and Lake Evolution of Southeastern Songliao Basin, NE China.Acta Palaeontologica Sinica, 48(3):556-568 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gswxb200903024 Xu, Z.Q., Wang, Q., Li, Z.H., et al., 2016.Indo-Asian Collision:Tectonic Transition from Compression to Strike Slip.Acta Geologica Sinica, 90(1):1-23 (in Chinese with English abstract). doi: 10.1111/1755-6724.12639 Zhang, C.H., Liu, J.S., Liu, D.L., 2006.Geological and Geochemical Characteristics and Tectonic Setting of Triassic Volcanic Suite in Guanfang Area along South Lancangjiang Belt.Acta Peirologica et Mineralogica, 25(5):377-386 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz200605002 Zhang, K.X., He, W.H., Luo, M.S., et al., 2017.The Deposition Construction and Sedimentary Tectonic in China.Geological Publishing House, Beijing (in Chinese). Zhang, W.T., Chen, P.J., Shen, Y.B., 1976.Fossil Conchostraca of China.Science Press, Beijing (in Chinese). Zhang, Y.Z., Zhang, D.H., Liu, S.R., et al., 1996.Lithology and Stratigraphy of Yunnan Province.China University of Geosciences Press, Wuhan (in Chinese). Zhang, Z., Song, J.L., Tang, J.X., et al., 2017.Petrogenesis, Diagenesis and Mineralization Ages of Galale Cu-Au Deposit, Tibet:Zircon U-Pb Age, Hf Istopic Compositon and Molybdenite Re-Os Dating.Earth Science, 42(6):862-880 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.523 Zhu, W.G., Zhong, H., Wang, L.Q., et al., 2011.Petrogenesis of the Basalts and Rhyolite Porphyries of the Minle Copper Deposit, Yunnan:Geochronological and Geochemical Constraints.Acta Petrologica Sinica, 27(9):2694-2708 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201109018 陈丕基, 2012.中国白垩纪叶肢介生物地层学.地层学杂志, 36(2):300-313. http://d.old.wanfangdata.com.cn/Conference/8237668 范蔚茗, 彭头平, 王岳军, 2009.滇西古特提斯俯冲-碰撞过程的岩浆作用记录.地学前缘, 16(6):291-302. doi: 10.3321/j.issn:1005-2321.2009.06.031 孔会磊, 董国臣, 莫宣学, 等, 2012.滇西三江地区临沧花岗岩的岩石成因:地球化学、锆石U-Pb年代学及Hf同位素约束.岩石学报, 28(5):1438-1452. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201205008 冷秋锋, 唐菊兴, 郑文宝, 等, 2016.西藏拉抗俄斑岩Cu-Mo矿床含矿斑岩地球化学、锆石U-Pb年代学及Hf同位素组成.地球科学, 41(6):999-1015. https://doi.org/10.3799/dqkx.2016.083 李罡, 陈丕基, 万晓樵, 等, 2004.嫩江阶底界层型剖面研究.地层学杂志, 28(4):297-299, 335. doi: 10.3969/j.issn.0253-4959.2004.04.002 李兴林, 1996.临沧复式花岗岩基的基本特征及形成构造环境的研究.云南地质, 15(1):1-18. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199600616589 廖焕宇, 黄迪颖, 2014.河北省青龙县霸王沟侏罗纪叶肢介化石.地层学杂志, 38(4):433-438. http://www.cqvip.com/QK/92920X/201404/662909294.html 刘昌实, 朱金初, 徐夕生, 1989.滇西临沧复式岩基特征研究.云南地质, 8(3-4):189-204. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK000003601932 罗亮, 安显银, 吴年文, 等, 2014.班公湖-双湖-怒江-昌宁-孟连新元古代-中生代沉积盆地演化.地球科学, 39(8):1169-1184. http://earth-science.net/WebPage/Article.aspx?id=2911 牛绍武, 李佩贤, 程政武, 等, 2005.滇中地区上侏罗统叶肢介化石及其地层学意义.地质通报, 24(4):329-340. doi: 10.3969/j.issn.1671-2552.2005.04.006 牛绍武, 田树刚, 庞其清, 2010.冀北滦平盆地大店子组叶肢介生物地层特征与陆相侏罗系-白垩系界线.地质通报, 29(7):961-979. doi: 10.3969/j.issn.1671-2552.2010.07.001 彭头平, 王岳军, 范蔚茗, 等, 2006.澜沧江南段早中生代酸性火成岩SHRIMP锆石U-Pb定年及构造意义.中国科学(D辑), 36(2):123-132. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200602002 王二七, 2017.关于印度与欧亚大陆初始碰撞时间的讨论.中国科学(D辑), 3(47):284-292. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QKC20172017041000086134 王硕, 董国臣, 莫宣学, 等, 2012.澜沧江南带三叠纪火山岩岩石学、地球化学特征、Ar-Ar年代学研究及其构造意义.岩石学报, 28(4):1148-1162. http://d.old.wanfangdata.com.cn/Conference/7667376 王思恩, 李罡, 2008.冀北、辽西地区上侏罗统土城子组的新叶肢介化石.古生物学报, 47(3):319-325. doi: 10.3969/j.issn.0001-6616.2008.03.007 韦诚, 戚学祥, 常裕林, 等, 2016.澜沧江构造带中南段小定西组火山岩形成时代的厘定及其构造意义.地质学报, 90(11):3192-3214. doi: 10.3969/j.issn.0001-5717.2016.11.014 席党鹏, 李罡, 万晓樵, 等, 2009.松辽盆地东南区姚家组-嫩江组一段地层特征与湖泊演变.古生物学报, 48(3):556-568. doi: 10.3969/j.issn.0001-6616.2009.03.024 许志琴, 王勤, 李忠海, 等, 2016.印度-亚洲碰撞:从挤压到走滑的构造转换.地质学报, 90(1):1-23. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201101001 张彩华, 刘继顺, 刘德利, 2006.滇西南澜沧江带官房地区三叠纪火山岩地质地球化学特征及其构造环境.岩石矿物学杂志, 25(5):377-386. doi: 10.3969/j.issn.1000-6524.2006.05.002 张克信, 何卫红, 骆满生, 等, 2017.中国沉积岩建造与沉积大地构造.北京:地质出版社. 张文堂, 陈丕基, 沈炎彬, 1976.中国的叶肢介化石.北京:科学出版社. 张远志, 张定辉, 刘世荣, 等, 1996.云南省岩石地层.武汉:中国地质大学出版社. 张志, 宋俊龙, 唐菊兴, 等, 2017.西藏嘎拉勒铜金矿床的成岩成矿时代与岩石成因:锆石U-Pb年龄、Hf同位素组成及辉钼矿Re-Os定年.地球科学, 42(6):862-880. https://doi.org/10.3799/dqkx.2017.523 中国科学院南京地质古生物研究所, 1974.西南地区地层古生物手册.北京:科学出版社. 朱维光, 钟宏, 王立全, 等, 2011.云南民乐铜矿床中玄武岩和流纹斑岩的成因:年代学和地球化学制约.岩石学报, 27(9):2694-2708. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201109018 -
点击查看大图
图(9) / 表(1)
计量
- 文章访问数: 4131
- HTML全文浏览量: 1778
- PDF下载量: 25
- 被引次数: 0
