东天山哈尔里克地区晚石炭世淡色花岗岩成因及其地质意义

朱小辉; 朱涛; 张欣; 奚任刚; 孟勇; 王凯

doi:10.3799/dqkx.2018.989

Volume 43 Issue 12

Dec. 2018

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2018 > 43(12): 4443-4458

Zhu Xiaohui, Zhu Tao, Zhang Xin, Xi Rengang, Meng Yong, Wang Kai, 2018. Petrogenesis and Geological Implications of Late Carboniferous Leucogranites in Harlik Area, Eastern Tianshan. Earth Science, 43(12): 4443-4458. doi: 10.3799/dqkx.2018.989

Citation:

Zhu Xiaohui, Zhu Tao, Zhang Xin, Xi Rengang, Meng Yong, Wang Kai, 2018. Petrogenesis and Geological Implications of Late Carboniferous Leucogranites in Harlik Area, Eastern Tianshan. Earth Science, 43(12): 4443-4458. doi: 10.3799/dqkx.2018.989

Citation:

Zhu Xiaohui, Zhu Tao, Zhang Xin, Xi Rengang, Meng Yong, Wang Kai, 2018. Petrogenesis and Geological Implications of Late Carboniferous Leucogranites in Harlik Area, Eastern Tianshan. Earth Science, 43(12): 4443-4458. doi: 10.3799/dqkx.2018.989

PDF( 3695 KB)

Petrogenesis and Geological Implications of Late Carboniferous Leucogranites in Harlik Area, Eastern Tianshan

doi: 10.3799/dqkx.2018.989

1.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Natural Resources, Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China
2.
State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China
3.
Department of Geology, Northwest University, Xi'an 710069, China

Received Date: 2018-03-23
Publish Date: 2018-12-15

Abstract

Abstract

The leucogranite provides key insights into the tectonic evolution of orogenic belt. Petrology, geochemistry and geochronology results show that there are four types of leucogranites in the Xiaopu area in the southern piedmont of the Harlik area, eastern Tianshan, including the biotite leucogranite, two-mica leucogranite, tourmaline-bearing leucogranite and garnet-bearing leucogranite. These leucogranites are rich in silica (SiO₂=73.22%-75.12%), aluminium (Al₂O₃=13.59%-14.49%), alkali(ALK=7.11%-9.67%), but low in titanium (TiO₂=0.01%-0.14%), iron(TFeO=0.26%-1.37%), magnesium (MgO=0.09%-0.46%) and calcium (CaO=0.46%-1.92%), which belong to the calc-alkaline to shoshonite peraluminous granite. The high CaO/Na₂O (0.46-0.47) and low Rb/Sr (0.31-0.33) ratios of the biotite leucogranite imply that it was formed by the biotite dehydration of greywacke, whereas the low CaO/Na₂O (0.11-0.31) and high Rb/Sr (1.41-3.75) ratios indicate that the two-mica and tourmaline-bearing leucogranites were formed by the muscovite dehydration of meta-pelitic-arenaceous sedimentary rocks, and the strong negative Eu anomalies and "seagull forms" REE patterns reveal that the garnet-bearing leucogranite belongs to highly fractionated granite. Considered the geological features and low initial temperature (T=637-644℃), the Xiaopu leucogranites were probably formed related to the exhumation of deep material, or extensional collapse of the orogen. Zircon U-Pb results show that the formation ages of biotite and tourmaline-bearing leucogranites are 308.5±2.2 Ma and 307.8±2.3 Ma, respectively. Combining with the previous data, it is suggested that the Harlik area was in extensional tectonic setting in the Late Carboniferous.
- LA-ICP-MS U-Pb dating,
- leucogranite,
- post-collision,
- Harlik area,
- geochemistry

FullText(HTML)

References(89)

References

Braun, I., Raith, M., Kumar, G.R.R., 1996.Dehydration-Melting Phenomena in Leptynitic Gneisses and the Generation of Leucogranites:A Case Study from the Kerala Khondalite Belt, Southern India.Journal of Petrology, 37(6):1285-1305. https://doi.org/10.1093/petrology/37.6.1285

Brown, M., 2002.Retrograde Processes in Migmatites and Granulites Revisited.Journal of Metamorphic Geology, 20(1):25-40. https://doi.org/10.1046/j.0263-4929.2001.00362.x

Cao, F.G., Tu, Q.J., Zhang, X.M., et al., 2006.Preliminary Determination of the Early Paleozoic Magmatic Arc in the Karlik Mountains, East Tianshan, Xinjiang, China-Evidence from Zircon SHRIMP U-Pb Dating of Granite Bodies in the Tashuihe Area.Geological Bulletin of China, 25(8):923-927 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200608004

Cao, F.G., Zhang, Y.P., Li, Y., et al., 2009.The Gelogical Character of Nanhuan System Qingshixia Formation Qincheng Hami, Xijiang.Xinjiang Geology, 27(4):303-307 (in Chinese with English abstract).

Chen, X.J., Shu, L.S., 2010.Features of the Post-Collisional Tectono-Magmatism and Geochronological Evidence in the Harlik Mt., Xinjiang.Acta Petrologica Sinica, 26(10):3057-3064 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB201010017.htm

Chen, X.J., Shu, L.S., Santosh, M., 2011.Late Paleozoic Post-Collisional Magmatism in the Eastern Tianshan Belt, Northwest China:New Insights from Geochemistry, Geochronology and Petrology of Bimodal Volcanic Rocks.Lithos, 127(3-4):581-598. https://doi.org/10.1016/j.lithos.2011.06.008

Chen, X.J., Zhang, K.H., Zhang, G.L., et al., 2016.Characteristics, Petrogenesis and Tectonic Implications of the Permian Omoertage Alkaline Granites in Harlik Area, Xinjiang.Acta Petrologica et Mineralogica, 35(6):929-946 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=yskwxzz201606002

Chung, S.L., Chu, M.F., Zhang, Y.Q., et al., 2005.Tibetan Tectonic Evolution Inferred from Spatial and Temporal Variations in Post-Collisional Magmatism.Earth-Science Reviews, 68(3-4):173-196.https://doi.org/10.1016/j.earscirev.2004.05.001 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=edd81f21a4b046d1678a4727beb6f78a

Gao, L.E., Zeng, L.S., 2014.Fluxed Melting of Metapelite and the Formation of Miocene High-CaO Two-Mica Granites in the Malashan Gneiss Dome, Southern Tibet.Geochimica et Cosmochimica Acta, 130:136-155. https://doi.org/10.1016/j.gca.2014.01.003

Gao, L.E., Zeng, L.S., Hu, G.Y., 2010.High Sr/Y Two-Mica Granite from Quedang Area, Southern Tibet, China:Formation Mechanism and Tectonic Implications.Geologcal Bulletin of China, 29(2):214-226 (in Chinese with English abstract).

Gao, L.E., Zeng, L.S., Liu, J., et al., 2009.Early Oligocene Na-Rich Peraluminous Leucogranites in the YardoiGneiss Dome, Southern Tibet:Formation Mechanism and Tectonic Implications.Acta Petrologica Sinica, 25(9):2289-2302 (in Chinese with English abstract).

Gao, L.E., Zeng, L.S., Asimow, P.D., 2016.Contrasting Geochemical Signatures of Fluid-Absent versus Fluid-Fluxed Melting of Muscovite in Metasedimentary Sources:The Himalayan Leucogranites.Geology, 45(1):39-42.https://doi.org/10.1130/g38336.1 http://adsabs.harvard.edu/abs/2017Geo....45...39G

Gu, L.X., Hu, S.X., Chu, Q., et al., 1999.Pre-Collision Granites and Post-Collision Intrusive Assemblage of the Kelameili-Harlik Orogenic Belt.Acta Geologica Sinica (English Edition), 73(3):316-329.https://doi.org/10.1111/j.1755-6724.1999.tb00840.x doi: 10.1111/acgs.1999.73.issue-3

Gu, L.X., Zhang, Z.Z., Wu, C.Z., et al., 2006.Some Problems on Granites and Vertical Growth of the Continental Crust in the Eastern Tianshan Mountains, NW China.Acta Petrologica Sinica, 22(5):1103-1120 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200605005

Guo, H.C., Zhong, L., Li, L.Q., 2006.Zircon SHRIMP U-Pb Dating of Quartz Diorite in the Koumenzi Area, Karlik Mountains, East Tianshan, Xinjiang, China, and Its Geological Significance.Geological Bulletin of China, 25(8):928-931 (in Chinese with English abstract).

Guo, S.S., Li, S.G., 2007.Petrological and Geochemical Constraints on the Origin of Leucogranites.Earth Science Frontiers, 14(6):290-298 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200706036

Harrison, M.T., Grove, M., Mckeegan, K.D., et al., 1999.Origin and Episodic Emplacement of the Manaslu Intrusive Complex, Central Himalaya.Journal of Petrology, 40(1):3-19. https://doi.org/10.1093/petroj/40.1.3

Hou, Z.Q., Zheng, Y.C., Zeng, L.S., et al., 2012.Eocene-Oligocene Granitoids in Southern Tibet:Constraints on Crustal Anatexis and Tectonic Evolution of the Himalayan Orogen.Earth and Planetary Science Letters, 349-350:38-52. https://doi.org/10.1016/j.epsl.2012.06.030

Inger, S., Harris, N., 1993.Geochemical Constraints on Leucogranite Magmatism in the Langtang Valley, Nepal Himalaya.Journal of Petrology, 34(2):345-368. https://doi.org/10.1093/petrology/34.2.345

King, J., Harris, N., Argles, T., et al., 2010.Contribution of Crustal Anatexis to the Tectonic Evolution of Indian Crust beneath Southern Tibet.Geological Society of America Bulletin, 123(1-2):218-239.https://doi.org/10.1130/b30085.1 doi: 10.1130-B30085.1/

Li, J.T., He, X.F., Liu, L., et al., 2017.Ordovician Tectonic Evolution of Harlik in Eastern Tianshan of Xinjiang:Constraints from LA-ICP-MS Zircon U-Pb Geochronology and Geochemistry of Volcanic Rocks.Geoscience, 31(3):460-473 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-XDDZ201703004.htm

Li, J.Y., 2004.Late Neoproterozoic and Paleozoic Tectonic Framework and Evolution of Eastern Xinjiang, NW China.Geological Review, 50(3):304-322 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp200403015

Li, J.Y., He, G.Q., Xu, X., et al., 2006.Crustal Tectonic Framework of Northern Xinjiang and Adjacent Regions and Its Formation.Acta Geologica Sinica, 80(1):148-168 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200601017

Liu, L., He, X.F., Li, J.T., et al., 2017.Petrogenesis and Tectonic Signficances of the Qincheng Tianshengquan Pluton in the Harlik Orogen of Eastern Xinjiang.Geological Science and Technology Information, 36(2):86-96 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZKQ201702011.htm

Liu, Z.C., Wu, F.Y., Ji, W.Q., et al., 2014.Petrogenesis of the Ramba Leucogranite in the Tethyan Himalaya and Constraints on the Channel Flow Model.Lithos, 208-209:118-136. https://doi.org/10.1016/j.lithos.2014.08.022

Luo, T., Chen, J.P., Liao, Q.A., et al., 2018.Geochronology, Geochemistry and Geological Significance of the Late Carboniferous Bimodal Volcanic Rocks in the Balikun Area, Eastern Tianshan.Earth Science, 43(9):3018-3035 (in Chinese with English abstract).https://doi.org/10.3799/dqkx.2018.603 http://d.old.wanfangdata.com.cn/Periodical/dqkx201809008

Ma, X.H., Chen, B., Wang, C., et al., 2015.Early Paleozoic Subduction of the Paleo-Asian Ocean:Zircon U-Pb Geochronological, Geochemical and Sr-Nd Isotopic Evidence from the Harlik Pluton, Xinjiang.Acta Petrologica Sinica, 31(1):89-104 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201501007

McDermott, F., Harris, N.B.W., Hawkesworth, C.J., 1996.Geochemical Constraints on Crustal Anatexis:A Case Study from the Pan-African Damara Granitoids of Namibia.Contributions to Mineralogy and Petrology, 123(4):406-423. https://doi.org/10.1007/s004100050165

Miller, C.F., McDowell, S.M., Mapes, R.W., 2003.Hot and Cold Granites? Implications of Zircon Saturation Temperatures and Preservation of Inheritance.Geology, 31(6):529.https://doi.org/10.1130/0091-7613(2003)031<0529:hacgio>2.0.co;2 doi: 10.1130/0091-7613(2003)031<0529:HACGIO>2.0.CO;2

Nabelek, P.I., Bartlett, C.D., 1998.Petrologic and Geochemical Links between the Post-Collisional Proterozoic Harney Peak Leucogranite, South Dakota, USA, and Its Source Rocks.Lithos, 45(1-4):71-85.https://doi.org/10.1016/s0024-4937(98)00026-7 doi: 10.1016/S0024-4937(98)00026-7

Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81.https://doi.org/10.1007/bf00384745 doi: 10.1007/BF00384745

Rickwood, P.C., 1989.Boundary Lines within Petrologic Diagrams which Use Oxides of Major and Minor Elements.Lithos, 22(4):247-263. https://doi.org/10.1016/0024-4937(89)90028-5

Şeng ör, 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

Song, P., Tong, Y., Wang, T., et al., 2018.Zircon U-Pb Ages, Genetic Evolution and Geological Significance of Carboniferous Granites in the Harlik Mountain, East Tianshan, Xinjiang.Geological Bulletin of China, 37(5):790-804 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/zgqydz201805004

Stevens, G., Clemens, J.D., Droop, G.T.R., 1997.Melt Production during Granulite-Facies Anatexis:Experimental Data from "Primitive" Metasedimentary Protoliths.Contributions to Mineralogy and Petrology, 128(4):352-370. https://doi.org/10.1007/s004100050314

Sun, G.H., 2007.Structural Deformation and Tectonic Evolution of Harlik Mountain, in Xinjiang since the Paleozoic(Dissertation).Chinese Academy of Geological Sciences, Beijing, 1-226 (in Chinese with English abstract).

Sun, G.H., Li, J.Y., Gao, L.M., et al., 2005.Zircon SHRIMP U-Pb Age of a Dioritic Pluton in the Harlik Mountain, Eastern Xinjiang, and Its Tectonic Implication.Geological Review, 51(4):463-469 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/OA000005244

Sun, G.H., Li, J.Y., Zhu, Z.X., et al., 2007a.Detrital Zircon SHRIMP U-Pb Dating of Carboniferous Sandstone from the Southern Foot of the Harlik Mountains, Eastern Xinjiang, and Its Geological Implications.Geology in China, 34(5):778-789 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi200705004

Sun, G.H., Li, J.Y., Zhu, Z.X., et al., 2007b.Zircons SHRIMP U-Pb Dating of Gneissoid-Biotitic Granite in Harlik Mountains, Eastern of Xinjiang and Its Geological Implications.Xinjiang Geology, 25(1):4-10 (in Chinese with English abstract).

Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345.https://doi.org/10.1144/gsl.sp.1989.042.01.19 doi: 10.1144/GSL.SP.1989.042.01.19

Sylvester, P.J., 1998.Post-Collisional Strongly Peraluminous Granites.Lithos, 45(1-4):29-44.https://doi.org/10.1016/s0024-4937(98)00024-3 doi: 10.1016/S0024-4937(98)00024-3

Wang, C., Ma, X.H., Chen, B., et al., 2017.Late Carboniferous Volcanism of the Harlik Orogenic Belt, Xinjiang:Zircon U-Pb Geochronological, Geochemical and Sr-Nd Isotopic Evidence.Acta Petrologica Sinica, 33(2):440-454 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTotal-YSXB201702009.htm

Wang, C.S., Gu, L.X., Zhang, Z.Z., et al., 2009a.Petrogenesis and Geological Implications of the Permian High-K Calc-Alkaline Granites in Harlik Mountains of Eastern Tianshan, NW China.Acta Petrologica Sinica, 25(6):1499-1511 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200906021

Wang, C.S., Gu, L.X., Zhang, Z.Z., et al., 2009b.Petrogenesis and Tectonic Implications of the Permian Alkaline Granite and Quartz-Syenite Assemblage in Harlik Mountains, Xinjiang.Acta Petrologica Sinica, 25(12):3182-3196 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200912007

Wang, L.Y., Liao, Q.A., Xiao, D., et al., 2016.Petrogenesis and Tectonic Significance of Early Carboniferous A-Type Granite in Harlik, Xinjiang.Journal of Geomechanics, 22(4):1032-1048 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlxxb201604020

Wang, X.X., Zhang, J.J., Wang, J.M., 2016.Geochronology and Formation Mechanism of the Paiku Granite in the Northern Himalaya, and Its Tectonic Implications.Earth Science, 41(6):982-998 (in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.082 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkx201606006

Wei, C.J., Wang, W., 2007.Phase Equilibria of Anatexis in High-Grade Metapelites.Earth Science Frontiers, 14(1):125-134 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200701012

Windley, B.F., Alexeiev, D., Xiao, W., et al., 2007.Tectonic Models for Accretion of the Central Asian Orogenic Belt.Journal of the Geological Society, 164(1):31-47. https://doi.org/10.1144/0016-76492006-022

Wu, F.Y., Liu, X.C., Ji, W.Q., et al., 2017.Highly Fractionated Granites:Recognition and Research.Science China Earth Sciences, 60(7):1201-1219. https://doi.org/10.1007/s11430-016-5139-1

Xiao, W., Windley, B.F., Badarch, G., et al., 2004.Palaeozoic Accretionary and Convergent Tectonics of the Southern Altaids:Implications for the Growth of Central Asia.Journal of the Geological Society, 161(3):339-342. https://doi.org/10.1144/0016-764903-165

Xie, K.J., Zeng, L.S., Liu, J., et al., 2010.Late-Eocene Dala Adakitic Granite, Southern Tibet and Geological Implications.Acta Petrologica Sinica, 26(4):1016-1026 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201004002

Zeng, L.S., Gao, L.E., 2017.Cenozoic Crustal Anatexis and the Leucogranites in the Himalayan Collisional Orogenic Belt.Acta Petrologica Sinica, 33(5):1420-1444 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201705004

Zhang, H.F., Harris, N., Parrish, R., et al., 2004.Causes and Consequences of Protracted Melting of the Mid-Crust Exposed in the North Himalayan Antiform.Earth and Planetary Science Letters, 228(1-2):195-212. https://doi.org/10.1016/j.epsl.2004.09.031

Zhang, H.F., Nigel, H., Randall, P., et al., 2005.Geochemistry of North Himalayan Leucogranites:Regional Comparison, Petrogenesis and Tectonic Implications.Earth Science, 30(3):275-288 (in Chinese with English abstract). http://cpfd.cnki.com.cn/Article/CPFDTOTAL-IGQM200408001058.htm

Zhao, M., Shu, L.S., Wang, C.Y., 1997.Characteristics of Metamorphism in the Harlik Metamorphic Belt, East Xinjiang, and Its Tectonic Environment.Geological Journal of China Universities, 3(1):40-50 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700148698

Zhao, M., Shu, L.S., Zhu, W.B., et al., 2002.Zircon U-Pb Dating of the Rocks from the Harlik Metamorphic Belt in Eastern Xinjiang and Its Geological Significance.Acta Geologica Sinica, 76(3):379-383 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200203010

Zhao, T.Y., Xu, S.Q., Zhu, Z.X., et al., 2014.Geological and Geochemical Features of Carboniferous Volcanic Rocks in Bogda-Harlik Mountains, Xinjiang and Their Tectonic Significances.Geological Review, 60(1):115-124 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-DZLP201401013.htm

曹福根, 涂其军, 张晓梅, 等, 2006.哈尔里克山早古生代岩浆弧的初步确定——来自塔水河一带花岗质岩体锆石SHRIMP U-Pb测年的证据.地质通报, 25(8):923-927. doi: 10.3969/j.issn.1671-2552.2006.08.004

曹福根, 张玉萍, 李艳, 等, 2009.新疆哈密沁城一带南华系青石峡组地质特征及意义.新疆地质, 27(4):303-307. doi: 10.3969/j.issn.1000-8845.2009.04.001

陈希节, 舒良树, 2010.新疆哈尔里克山后碰撞期构造-岩浆活动特征及年代学证据.岩石学报, 26(10):3057-3064. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201010017

陈希节, 张奎华, 张关龙, 等, 2016.新疆东天山哈尔里克二叠纪奥莫尔塔格碱性花岗岩特征、成因及构造意义.岩石矿物学杂志, 35(6):929-946. doi: 10.3969/j.issn.1000-6524.2016.06.002

高利娥, 曾令森, 胡古月, 2010.藏南确当地区高Sr/Y比值二云母花岗岩的形成机制及其构造动力学意义.地质通报, 29(2):214-226. doi: 10.3969/j.issn.1671-2552.2010.02.005

高利娥, 曾令森, 刘静, 等, 2009.藏南也拉香波早渐新世富钠过铝质淡色花岗岩的成因机制及其构造动力学意义.岩石学报, 25(9):2289-2302. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200909021

顾连兴, 张遵忠, 吴昌志, 等, 2006.关于东天山花岗岩与陆壳垂向增生的若干认识.岩石学报, 22(5):1103-1120. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605005

郭华春, 钟莉, 李丽群, 2006.哈尔里克山口门子地区石英闪长岩锆石SHRIMP U-Pb测年及其地质意义.地质通报, 25(8):928-931. doi: 10.3969/j.issn.1671-2552.2006.08.005

郭素淑, 李曙光, 2007.淡色花岗岩的岩石学和地球化学特征及其成因.地学前缘, 14(6):290-298. doi: 10.3321/j.issn:1005-2321.2007.06.036

李江涛, 何学锋, 刘亮, 等, 2017.新疆东天山哈尔里克奥陶纪的构造属性:来自火山岩LA-ICP-MS锆石U-Pb年代学与地球化学的制约.现代地质, 31(3):460-473. doi: 10.3969/j.issn.1000-8527.2017.03.004

李锦轶, 2004.新疆东部新元古代晚期和古生代构造格局及其演变.地质论评, 50(3):304-322. doi: 10.3321/j.issn:0371-5736.2004.03.015

李锦轶, 何国琦, 徐新, 等, 2006.新疆北部及邻区地壳构造格架及其形成过程的初步探讨.地质学报, 80(1):148-168. doi: 10.3321/j.issn:0001-5717.2006.01.017

刘亮, 何学锋, 李江涛, 等, 2017.新疆东部哈尔里克造山带沁城天生圈岩体岩石成因及其构造意义.地质科技情报, 36(2):86-96. http://www.cqvip.com/QK/93477A/201702/671732067.html

罗婷, 陈继平, 廖群安, 等, 2018.东天山巴里坤地区晚石炭世双峰式火山岩年代学、地球化学及其构造意义.地球科学, 43(9):3018-3035. http://earth-science.net/WebPage/Article.aspx?id=3937

马星华, 陈斌, 王超, 等, 2015.早古生代古亚洲洋俯冲作用:来自新疆哈尔里克侵入岩的锆石U-Pb年代学、岩石地球化学和Sr-Nd同位素证据.岩石学报, 31(1):89-104. http://d.wanfangdata.com.cn/Periodical/ysxb98201501007

宋鹏, 童英, 王涛, 等, 2018.新疆东天山哈尔里克山石炭纪花岗岩锆石U-Pb年龄、成因演化及地质意义.地质通报, 37(5):790-804. http://d.old.wanfangdata.com.cn/Periodical/zgqydz201805004

孙桂华, 2007.新疆哈尔里克山古生代以来构造变形及构造演化(博士学位论文).北京:中国地质科学院, 1-226.

孙桂华, 李锦轶, 高立明, 等, 2005.新疆东部哈尔里克山闪长岩锆石SHRIMP U-Pb定年及其地质意义.地质论评, 51(4):463-469. doi: 10.3321/j.issn:0371-5736.2005.04.015

孙桂华, 李锦轶, 朱志新, 等, 2007a.新疆东部哈尔里克山南麓石炭纪砂岩碎屑锆石SHRIMP U-Pb定年及其地质意义.中国地质, 34(5):778-789. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi200705004

孙桂华, 李锦轶, 朱志新, 等, 2007b.新疆东部哈尔里克山片麻状黑云母花岗岩锆石SHRIMP U-Pb定年及其地质意义.新疆地质, 25(1):4-10. http://d.old.wanfangdata.com.cn/Periodical/xjdz200701002

王超, 马星华, 陈斌, 等, 2017.新疆哈尔里克山地区晚石炭世火山作用:锆石U-Pb年代学、元素地球化学及Sr-Nd同位素研究.岩石学报, 33(2):440-454. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201702009

汪传胜, 顾连兴, 张遵忠, 等, 2009a.东天山哈尔里克山区二叠纪高钾钙碱性花岗岩成因及地质意义.岩石学报, 25(6):1499-1511. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200906021

汪传胜, 顾连兴, 张遵忠, 等, 2009b.新疆哈尔里克山二叠纪碱性花岗岩-石英正长岩组合的成因及其构造意义.岩石学报, 25(12):3182-3196. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200912007

王良玉, 廖群安, 肖典, 等, 2016.新疆哈尔里克早石炭世A型花岗岩的岩石成因及构造意义.地质力学学报, 22(4):1032-1048. doi: 10.3969/j.issn.1006-6616.2016.04.020

王晓先, 张进江, 王佳敏, 2016.北喜马拉雅佩枯花岗岩年代学、成因机制及其构造意义.地球科学, 41(6):982-998. http://earth-science.net/WebPage/Article.aspx?id=3311

魏春景, 王伟, 2007.高级变质岩中深熔作用的相平衡研究.地学前缘, 14(1):125-134. doi: 10.3321/j.issn:1005-2321.2007.01.012

谢克家, 曾令森, 刘静, 等, 2010.西藏南部晚始新世打拉埃达克质花岗岩及其构造动力学意义.岩石学报, 26(4):1016-1026. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201004002

曾令森, 高利娥, 2017.喜马拉雅碰撞造山带新生代地壳深熔作用与淡色花岗岩.岩石学报, 33(5):1420-1444. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201705004

张宏飞, Nigel, H., Randall, P., 等, 2005.北喜马拉雅淡色花岗岩地球化学:区域对比、岩石成因及其构造意义.地球科学, 30(3):275-288. http://earth-science.net/WebPage/Article.aspx?id=1410

赵明, 舒良树, 王赐银, 1997.东疆哈尔里克变质地带变质作用特征及形成构造环境研究.高校地质学报, 3(1):40-50. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700148698

赵明, 舒良树, 朱文斌, 等, 2002.东疆哈尔里克变质带的U-Pb年龄及其地质意义.地质学报, 76(3):379-383. doi: 10.3321/j.issn:0001-5717.2002.03.010

赵同阳, 徐仕琪, 朱志新, 等, 2014.新疆博格达-哈尔里克山地区石炭纪火山岩地质地球化学特征及其构造意义.地质论评, 60(1):115-124. http://www.cnki.com.cn/Article/CJFDTotal-DZLP201401013.htm

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(7) / Tables(2)

Get Citation

PDF

XML

Article views (4774) PDF downloads(56)

Petrogenesis and Geological Implications of Late Carboniferous Leucogranites in Harlik Area, Eastern Tianshan

doi: 10.3799/dqkx.2018.989

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content