From source to sink: Coupling relation between the Dabie Shan Orogen provenance and Mesozoic sediments of the south-margin of Hefei Basin, based on the evidence of detrital zircon ages
Li Shuang-Ying, Wei Xing, Xie Wei, Cheng Cheng, Li Min, Hu Bo, Chai Guang-Lu
School of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009,China
Abstract：The Dabie Orogen formed in Triassic and its peripheral Mesozoic basins form a source to sink system.The Hefei Basin with well-developed Mesozoic in the north and well-exposed outcrops in the south provides ideal sedimentary records for the investigation of the basin-ridge source to sink system. Ten sandstone and one conglomerate samples were collected for zircon U-Pb(LA-ICP-MS)dating analysis which result in 742 effective ages(confidence level larger or equal to 85%)ranging from 113 Ma to 2983 Ma. The detrital zircon ages can be divided into five age groups,including 113-137 Ma and with a peak of 131 Ma,184-273 Ma and with a peak of 226 Ma,274-517.3 Ma and with two peaks of 280 Ma and 474 Ma,532-856.6 Ma and with three peaks of 572 Ma,649 Ma and 772 Ma,1786-2600 Ma and with two peaks of 2035 Ma and 2506 Ma. Moreover,we summarized the zircon U-Pb age data of various geological terrains from the Dabie Orogen and comparised the data with the aforementioned five age groups. Based on the zircon U/Pb ages and their Th/U ratios,the five age groups correctly correspond to the provenance geological terrains that are respectively Early Cretaceous magma rocks,Dabie Shan HP-UHP metamorphic rocks,north Huaiyang lower-grade metamorphic rocks,north Dabie orthogneiss and Luzhengguan group metamorphic rocks. According to the youngest zircon U-Pb ages,the Mesozoic stratigraphic framework of the south margin of the Hefei Basin is newly amended,which supports a time frame for source to sink system research. Mesozoic sedimentation in the south margin of the Hefei Basin can be divided into four evolutive stages (i.e., Later Triassic Rhaetian-Early Jurassic Sinemurian,Middle-Later Jurassic,early and Later stages of Early Cretaceous),and major characters and space-time changes of source rocks in each stage also are determined. Detrital zircon U/Pb ages and Th/U ratios suggest that the UHP process happened in the Dabie Orogen to Triassic,not Caledonian or Neoproterozoic. It was in Late Triassic Rhaetian that UHP rocks exhumated and outcropped in surface,and it was Neoproterozoic that the paleo-inland arc of the Dabie Orogen developed. Results from the present study contribute to rebuild tectonic palaeogeography of the Dabie Orogen and provide a case for study of basin-ridge source to sink system.
Li Shuang-Ying,Wei Xing,Xie Wei et al. From source to sink: Coupling relation between the Dabie Shan Orogen provenance and Mesozoic sediments of the south-margin of Hefei Basin, based on the evidence of detrital zircon ages[J]. JOPC, 2019, 21(1): 82-106.
1 安徽省地质矿产局. 1987. 安徽省区域地质志. 北京: 地质出版社,721. [Anhui Bureau of Geology and Mineral Resources. 1987. Regional Geology of Anhui Province. Beijing: Geological Publishing House,721] 2 安徽省地质矿产局. 1997. 安徽省岩石地层. 湖北武汉: 中国地质大学出版社,198-206. [Anhui Bureau of Geology and Mineral Resources. 1997. Stratigraphy of Anhui Province. Wuhan of Hubei: China University of Geosciences Press,198-206] 3 陈道公,倪涛. 2004. 大别—苏鲁造山带高级变质岩中锆石微区U,Th和Pb化学组成特征统计. 岩石学报, 20(5): 999-1006. [Chen D G,Ni T.2004. Zircon U,Th and Pb characteristics of high-grade metamorphic rocks from Dabie-Sulu orogen. Acta Petrologica Sinica, 20(5): 999-1006] 4 程裕淇,刘敦一,Williams I S,简平,庄育勋,高天山. 2000. 大别山碧溪岭深色榴辉岩和片麻状花岗质岩石SHRIMP分析. 地质学报, 74(3): 193-205. [Cheng Y Q,Liu D Y,Williams I S,Jian P,Zhuang Y X,Gao T S.2000. SHRIMP U-Pb dating of zircons of a dark-coloured eclogite and a garnet-bearing gneissic-granitic rock from Bixiling,eastern Dabie area. Acta Geologica Sinica, 74(3): 193-205] 5 高道明,吴维平. 2008. 大别山南部宿松群的组成及形成时代. 安徽地质, 18(2): 85-93. [Gao D M,Wu W P.2008. Formation and ages of Susong Group in the south of the Dabie Mountains. Anhui Geology, 18(2): 85-93] 6 韩树芬. 1996. 安徽北部中新生代沉积盆地分析. 北京: 地质出版社,127. [Han S F.1996. Mesozoic and Cenozoic Sedimentary Basins in Northern Anhui. Beijing: Geological Publishing House,127] 7 黄皓,薛怀民. 2012. 北淮阳早白垩世金刚台组火山岩LA-ICP-MS锆石U-Pb年龄及其地质意义. 岩石矿物学杂志, 31(3): 371-381. [Huang H,Xue H M.2012. LA-ICP-MS zircon U-Pb ages of Early Cretaceous volcanic rocks from Jingangtai Formation in Beihuaiyang belt on the northern margin of the Dabie Orogen and their geological implications. Acta Petrologica et Mineralogica, 31(3): 371-381] 8 简平,杨巍然,李志昌,周慧芳. 1997. 大别山西部熊店加里东期榴辉岩:同位素地质年代学的证据. 地质学报, 71(2): 133-140. [Jian P,Yang W R,Li Z C,Zhou H F.1997. Isotopic geochronological evidence for the caledonian Xiongdian eclogite in the western Dabie Mountains,China. Acta Geologica Sinica, 71(2): 133-140] 9 江来利,吴维平,刘贻灿,李惠民. 2003. 大别山南部宿松杂岩的U-Pb锆石和Ar-Ar角闪石年龄及其地质意义. 岩石学报, 19(3): 497-505. [Jiang L L,Wu W P,Liu Y C,Li H M.2003. U-Pb zircon and Ar-Ar hornblende ages of the Susong complex of the southern Dabie orogen and their geological implication. Acta Petrologica Sinica, 19(3): 497-505] 10 李俊辉,于洋,韦龙猛,胡昭平,陈福坤. 2016. 大别山造山带宿松岩群锆石U-Pb年龄和Nd同位素特征: 宿松地体物源和属性. 地球科学与环境学报, 38(1): 21-33. [Li J H,Yu Y,Wei L M,Hu Z P,Chen F K.2016. Zircon U-Pb ages and Nb isotopic characteristics of Susong Group in Dabie orogenic belt: Source and provenance of Susong terrane. Journal of Geosciences and Environment, 38(1): 21-33] 11 李任伟,李忠,江茂生,孙枢,金福全,张文华. 2000. 合肥盆地碎屑石榴石组成及其对源区恢复和地层对比的意义. 中国科学: 地球科学,30(s1): 91-98. [Li R W,Li Z,Jiang M S,Sun S,Jin F Q,Zhang W H.2000. Composition of detrital garnet in Hefei Basin and its significance to source area restoration and stratigraphic correlation. Science in China: Earth Sciences,30(s1): 91-98] 12 李任伟,孙枢,李忠,江茂生,金福全,李双应. 2002. 高压—超高压岩石对合肥盆地侏罗系沉积的贡献. 岩石学报, 18(4): 526-530. [Li R W,Sun S,Li Z,Jiang M S,Jin F Q,Li S Y.2002. Contribution of high-pressure and ultrahigh-pressure rocks to the Jurassic sedimentation in Hefei Basin. Acta Petrologica Sinica, 18(4): 526-530] 13 李任伟,孟庆任,李双应. 2005. 大别山及邻区侏罗和石炭纪时期盆—山耦合: 来自沉积记录的认识. 岩石学报, 21(4): 1133-1143. [Li R W,Meng Q R,Li S Y.2005. Coupling of Jurassic and Carboniferous basins with the orogens in the Dabie Shan and adjacent area: Constraints from sedimentary record. Acta Petrologica Sinica, 21(4): 1133-1143] 14 李曙光,李秋立,侯振辉. 2005. 大别山超高压变质岩的年代学及冷却史. 见: 大别山超高压变质作用与碰撞造山带动力学编写组. 大别山超高压变质作用与碰撞造山带动力学. 北京: 科学出版社,64-117. [Li S G,Li Q L,Hou Z H.2005. Chronlogy and cooling history of the ultra-high pressure metamorphic rocks in the Dabie Shan. In: Editing board of ultrahigh-pressure metamorphism and collisional dynamics of the Dabie Mountains. Ultrahigh-pressure Metamorphism and Collisional Dynamics of the Dabie Mountains. Beijing: Science Press,64-117] 15 李双应,岳书仓,王道轩,刘因,王清晨,李任伟. 2002a. 大别造山带超高压变质岩折返隆升的地层学证据: 毛坦厂组榴辉岩砾石的启示. 地质论评, 48(4): 345-352. [Li S Y,Yue S C,Wang D X,Liu Y,Wang Q C,Li R W.2002a. Stratigraphic evidence of the exhumation and uplift of ultrahigh-pressure metamorphic rocks in the Dabie orogenic belt: Enlightenment from eclogite gravels in the Maotanchang Formation. Geological Review, 48(4): 345-352] 16 李双应,岳书仓,王道轩,刘因,李任伟,孟庆任,金福全. 2002b. 大别造山带北缘中生代地层格架厘定. 地层学杂志, 26(3): 178-186. [Li S Y,Yue S C,Wang D X,Liu Y,Li R W,Meng Q R,Jin F Q.2002b. On the framework of Mesozoic strata on the northern margin of Dabie Orogenic Belt. Journal of Stratigraphy, 26(3): 178-186] 17 李双应,李任伟,王道轩,刘因,岳书仓,孟庆任,金福全. 2004a. 大别山北缘早白垩世黑石渡组沉积体系研究. 沉积学报, 22(4): 566-572. [Li S Y,Li R W,Wang D X,Liu Y,Yue S C,Meng Q R,Jin F Q.2004a. Depositional system of Early Cretaceous Heishidu Formation in the north margin of the Dabie mountains. Acta Sedimentologica Sinica, 22(4): 566-572] 18 李双应,李任伟,岳书仓,王道轩,刘因,孟庆任,金福全. 2004b. 安徽肥西中生代碎屑岩地球化学特征及其对物源制约. 岩石学报, 20(3): 667-676. [Li S Y,Li R W,Yue S C,Wang D X,Liu Y,Meng Q R,Jing F Q.2004b. Geochemistry of Mesozoic detrital rocks and its constraints on provenance in Feixi area,Anhui Provence. Acta Petrologica Sinica, 20(3): 667-676] 19 李双应,王道轩,刘因,李任伟,孟庆任,岳书仓,金福全. 2005a. 合肥—潢川盆地南缘中生代冲积沉积及其构造意义. 地质学报, 79(4): 465-474. [Li S Y,Wang D X,Liu Y,Li R W,Meng Q R,Yue S C,Jin F Q.2005a. Mesozoic alluvial deposition on the southern margin of the Hefei-Huangchuan Basin and its tectonic implication. Acta Geologica Sinica, 79(4): 465-474] 20 李双应,李任伟,王道轩,刘因,孟庆任,岳书仓,金福全. 2005b. 大别山北缘凤凰台组砾石地球化学特征及源区构造环境. 沉积学报, 23(3): 380-388. [Li S Y,Li R W,Wang D X,Liu Y,Meng Q R,Yue S C,Jin F Q.2005b. Geochemistry of the conglomerates and the tectonic setting of their provenance in Fenghuangtai Formation in the north margin of the Dabie mountains. Acta Sedimentologica Sinica, 23(3): 380-388] 21 李忠,李任伟,孙枢,江茂生,张文华. 1999. 合肥盆地南部侏罗系砂岩碎屑组分及其物源构造属性. 岩石学报, 15(3): 438-445. [Li Z,Li R W,Sun S,Jiang M S,Zhang W H.1999. Detrital composition and provenance tectonic attributes of Jurassic sandstones,south Hefei Basin. Acta Petrologica Sinica, 15(3): 438-445] 22 李忠,李任伟,孙枢,张文华. 2001. 大别地块北缘侏罗系花岗岩类砾石的Rb-Sr年代学特征. 科学通报, 46(7): 582-585. [Li Z,Li R W,Sun S,Zhang W H.2001. Rb-Sr chronological characteristics of Jurassic granitoid gravels in the northern margin of the Dabie Block. Chinese Science Bulletin, 46(7): 582-585] 23 李忠,高剑. 2016. 构造活动区特征源汇体系及古地理重建: 以塔里木块体北缘记录“泛非”事件的碎屑锆石分析为例. 古地理学报, 18(2): 424-440. [Li Z,Gao J.2016. Characteristic source-sink systems and palaeogeographic reconstruction in an active tectonic region: A case research on detrital zircons recording the Pan-African event in northern Tarim Block. Journal of Palaeogeography(Chinese Edition), 18(2): 424-440] 24 刘景波,张灵敏,叶凯,苏文,程南飞. 2013. 大别山北部卢镇关群变质火山岩和共生变质的花岗岩全岩和锆石氧同位素、锆石U-Pb 年代学研究. 岩石学报, 29(5): 1511-1524. [Liu J B,Zhang L M,Ye K,Su W,Cheng N F.2013. Oxygen isotopes of whole-rock and zircon and zircon U-Pb ages of meta-rhyolite from the Luzhenguan Group and associated meta-granite in the northern Dabie Mountains. Acta Petrologica Sinica, 29(5): 1511-1524] 25 马昌前,明厚利,杨坤光. 2004. 大别山北麓的奥陶纪岩浆弧: 侵入岩年代学和地球化学证据. 岩石学报, 20(3): 393-402. [Ma C Q,Ming H L,Yang K G.2004. An Ordovician magmatic arc at the northern foot of Dabie mountains: Evidence from geochronology and geochemistry of intrusive rocks. Acta Petrologica Sinica, 20(3): 393-402] 26 孟庆任,李任伟,李双应. 2005. 中生代合肥盆地南部的沉积过程与大别山变质地体的剥露. 岩石学报, 21(4): 1145-1156. [Meng Q R,Li R W,Li S Y.2005. Mesozoic sedimentation of the southern Hefei Basin and exhumation of the Dabieshan metamorphic terrane. Acta Petrologica Sinica, 21(4): 1145-1156] 27 王道轩,金福全,谢宪德,刘因. 2000. 合肥盆地三尖铺组 40Ar-39Ar 同位素年代地层学研究. 地层学杂志, 24(3): 236-242. [Wang D X,Jin F Q,Xie X D,Liu Y.2000. Studies of 40Ar-39Ar isotopic chronostratigraphy of the Sanjianpu Formation in the Hefei Basin,Anhui. Journal of Stratigraphy, 24(3): 236-242] 28 王清晨,从柏林. 1998. 大别山超高压变质带的大地构造框架. 岩石学报, 14(4): 481-492. [Wang Q C,Cong B L.1998. Tectonic framework of the Dabieshan ultrahigh pressure metamorphic belt. Acta Petrologica Sinica, 14(4): 481-492] 29 汪品先. 2009. 深海沉积与地球系统. 海洋地质与第四纪地质, 29(4): 1-11. [Wang P X.2009. Deep sea sediments and earth system. Marine Geology & Quaternary Geology, 29(4): 1-11] 30 吴利仁,徐贵忠. 1998. 东秦岭—大别山碰撞造山带的地质演化. 北京: 科学出版社,177-183. [Wu L R,Xu G Z.1998. Geological Evolution of the East Qinling-Dabie Mountain Collision Orogenic Belt. Beijing: Science Press,177-183] 31 吴元保,陈道公,Deloule E,夏群科,李彬贤,程昊. 2001. 北大别片麻岩的锆石U-Pb年龄离子探针测定及其地质意义. 地质论评, 47(3): 239-243. [Wu Y B,Chen D G,Deloule E,Xia Q K,Li B X,Cheng H.2001. Zircon U-Pb ion probe ages of gneisses from northern Dabie Terrain and their geological implications. Geological Review, 47(3): 239-243] 32 吴元保,郑永飞,龚冰,唐俊,赵子福,查向平. 2004. 北淮阳卢镇关群岩浆岩锆石U-Pb年龄和氧同位素组成. 岩石学报, 20(5): 1007-1024. [Wu Y B,Zheng Y F,Gong B,Tang J,Zhao Z F,Zha X P.2004. Zircon U-Pb ages and oxygen isotope compositions of the Luzhenguan magmatic complex in the Beihuaiyang zone. Acta Petrologica Sinica, 20(5): 1007-1024] 33 徐嘉炜. 1981. 初论大别山碰撞带. 合肥工业大学学报, 4(3): 82-94. [Xu J W.1981. A preliminary study on the collision belt of Dabie Mts of East China. Journal of Hefei Polytechnic University, 4(3): 82-94] 34 徐树桐,刘贻灿,江来利. 1994. 大别山的构造格局和演化. 北京: 科学出版社. [Xu S T,Liu Y C,Jiang L L.1994. Tectonic Pattern and Evolution of the Dabie Mountains. Beijing: Science Press] 35 徐树桐,刘贻灿,江来利. 2003. 大别山造山带的构造几何学和运动学. 安徽合肥: 中国科学技术大学出版社. [Xu S T,Liu Y C,Jiang L L.2003. Tectonic Geometry and Kinematics of the Dabie Orogenic Belt. Hefei of Anhui: Press of University of Science and Technology of China] 36 许志琴,杨经绥,李海兵,姚建新. 2006. 中央造山带早古生代地体构架与高压/超高压变质带的形成. 地质学报, 80(12): 1793-1806. [Xu Z Q,Yang J S,Li H B,Yao J X.2006. The Early Paleozoic terrane framework and the formation of the high-pressure(HP)and ultra-high pressure(UHP)metamorphic belts at the central orogenic belt(COB). Acta Geologica Sinica, 80(12): 1793-1806] 37 薛怀民,董树文,刘晓春. 2002. 大别山东部花岗片麻岩的锆石U-Pb年龄. 地质科学, 37(2): 165-173. [Xue H M,Dong S W,Liu X C.2002. U/Pb zircon dating of granitic gneisses in eastern Dabie mountains,central China. Scientia Geologica Sinica, 37(2): 165-173] 38 杨巍然,王国灿,简平. 2000. 大别造山带构造年代学. 湖北武汉: 中国地质大学出版社. [Yang W R,Wang G C,Jian P.2000. Study on the Tectono-chronology of the Dabie Orogenic Belt. Wuhan of Hubei: China University of Geosciences Press] 39 杨祝良,沈加林,沈渭洲,谢方贵,陶奎元. 2002. 大别山北缘中生代火山—侵入岩锶—钕同位素组成特征及其物质来源. 岩石矿物学杂志, 21(3): 223-230. [Yang Z L,Shen J L,Shen W Z,Xie F G,Tao K Y.2002. Sr and Nd isotopic composition and material sources of Mesozoic volcano-intrusive rocks in the northern margin of Dabie Mountains. Acta Petrologica et Mineralogica, 21(3): 223-230] 40 游振东,钟增球,张泽明. 1999. 桐柏—大别山区高压变质相的构造配置. 地学前缘, 6(4): 237-245. [You Z D,Zhong Z Q,Zhang Z M.1999. The tectonic distribution of high-pressure metamorphic facies in Tongbai-Dabieshan,central China. Earth Science Frontiers, 6(4): 237-245] 41 赵子福,郑永飞,魏春生,吴元保. 2004. 大别山中生代中酸性岩浆岩锆石U-Pb定年、元素和氧同位素地球化学研究. 岩石学报,20(5): 1151-1174. [Zhao Z F,Zheng Y F,Wei C S,Wu Y B.2004. Zircon U-Pb age,element and oxygen isotope geochemistry of Mesozoic intermediate-felsic rocks in the Dabie Mountains. Acta Petrologica Sinica, 20(5): 1151-1174] 42 郑祥身,金成伟,翟明国,石永红. 1999. 北大别灰色片麻岩的岩石化学特征及大地构造背景. 岩石学报, 15(3): 350-358. [Zheng X S,Jin C W,Zhai M G,Shi Y H.1999. Petrochemistry and tectonic background of the gray gneisses in north Dabie terrane. Acta Petrologica Sinica, 15(3): 350-358] 43 周存亭,汤加富,高天山,童劲松,鲁如魁. 1995. 大别山地区片麻岩套的建立与成岩时代讨论. 安徽地质, 5(3): 29-40. [Zhou C T,Tang J F,Gao T S,Tong J S,Lu R K.1995. The establishment of gneiss suite and diagenetic time discussion,the Dabie Mt. Geology of Anhui, 5(3): 29-40] 44 Allen P A.2008. From landscapes into geological history. Nature, 451: 274-276 45 Babault J,Marc V M,Legrand X,Driessche J V D,Manuel G Q,Mudd S M.2018. Source-to-sink constraints on tectonic and sedimentary evolution of the western central range and Cenderawasih Bay(Indonesia). Journal of Asian Earth Sciences, 156: 265-287. 46 Bryant D L,Ayers J C,Gao S,Miller C F,Zhang H.2004. Geochemical,age,and isotopic constraints on the location of the Sino-Korean/Yangtze suture and evolution of the northern Dabie complex,east central China. Geological Society of America Bulletin, 116(5): 698-717. 47 Chen F K,Guo J H,Jiang L L,Siebel W,Cong B,Satir M.2004. Provenance of the Beihuaiyang lower-grade metamorphic zone of the Dabie ultrahigh-pressure collisional orogen,China: Evidence from zircon ages. Journal of Asian Earth Sciences, 22(4): 343-352. 48 Chen N S,You Z D,Suo S T,Yang Y,Li H M.1996. U-Pb zircon ages of intermediate granulites and deformed granites in Dabie Mountains,central China. Chinese Science Bulletin, 41(22): 1887-1890. 49 Chen R X,Ding B H,Zheng Y F,Hu Z C.2015. Multiple episodes of anatexis in a collisional orogen: Zircon evidence from migmatite in the Dabie orogen. Lithos, 212-215: 247-265. 50 Cheng F S,Fu T.2016. Source to sink relation between the Eastern Kunlun Range and the Qaidam Basin,northern Tibetan Plateau,during the Cenozoic. Geological Society of America Bulletin, 128(1-2): 258-283. 51 Covault J A,Romans B W,Graham S A,Andrea F,George E H.2011. Terrestrial source to deep-sea sink sediment budgets at high and low sea levels: Insights from tectonically active Southern California. Geology, 39: 619-622. 52 Dickinson W R,Gehrels G E.2009. Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata: A test against a Colorado Plateau Mesozoic database. Earth and Planetary Science Letters, 288: 115-125. 53 Dong S W,Sun X R,Zhang Y,Huang D Z,Dai S K,Yu B C.1993. The basic structures of the Dabie mountain collision orogenic belt. Chinese Science Bulletin, 38(22): 1884-1888. 54 Ernst W G,Zhou G,Liou J G,Eide E,Wang X.1991. High-pressure and superhigh-pressure metamorphic terranes in the Qinling-Dabie mountain belt,central China: Early- to mid-Phanerozoic accretion of the western paleo-Pacific Rim. Pacific Science Association Information Bulletin, 43: 6-15. 55 Faure M,Lin W,Shu L S,Sun Y,Scharur U.1999. Tectonics of the Dabieshan(eastern China)and possible exhumation mechanism of ultra high-pressure. Terra Nova, 11(6): 251-258. 56 Faure M,Lin W,le Breton N.2001. Where is the North China and South China block boundary in eastern China?Geology, 29: 119-122. 57 Gao S,Zhang B R,Gu X M,Xie Q L,Guo X M.1991. Sedimentary geochemical evidence of Silurian-Devonian docking between North China and Yangtze Plate. Science in China: Series B, 34(11): 1372-1380. 58 Garzanti E,Resentini A.2012. Forward compositional modelling of Alpine orogenic sediments. Sedimentary Geology, 280: 149-164. 59 Griffin W L,Belousova E A,Shee S R,Pearson N J,O'Reilly S Y.2004. Archean crustal evolution in the northern Yilarn Craton: U-Pb and Hf-isotope evidence from detrital zircons. Precambrian Research, 131(3-4): 231-282. 60 Grimmer J C,Lother R,Michael M,Franz L,Gaitzsch I,Tichomirowa M,Hacker B R,Zhang Y Q.2003. When did the ultrahigh-pressure rocks reach the surface?A 207Pb-206Pb zircon, 40Ar/39Ar white mica,Si-in-white mica,single-grain provenance study of Dabie Shan synorogenic foreland sediments. Chemical Geology, 197: 87-110. 61 Gu X F,Liu Y C,Deng L P.2013. Geochronology and petrogenesis of eclogite from the Luotian dome,North Dabie complex zone(central China),and their element and isotope behavior during exhumation. Chinese Science Bulletin, 58: 2132-2137. 62 Hacker B R,Ratschbacher L,Webb L,Ireland T,Walker D,Dong S W.1998. U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie orogen,China. Earth and Planetary Science Letters, 161: 215-230. 63 Hacker B R,Ratschbacher L,Webb L,McWilliams M O,Ireland T,Calvert A,Dnong S,Wenk H R,Chateigner D.2000. Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing. Journal of Geophysical Research,105(B6): 13339-13364. 64 Jiang L L,Siebel W,Chen F K,Liu Y C,Chu X D.2005. U-Pb zircon ages for the Luzhenguan Complex in northern part of the eastern Dabie orogen. Science in China: Earth Sciences, 48(9): 1357-1367. 65 Li R W,Sang H Q,Zhang R H,Chu Z Y,Li S Y,Jin F Q,Jiang M S.2003a. Geochronology of source materials from high-pressure and ultrahigh-pressure metamorphic rocks in Jurassic sedimentary rocks of Hefei Basin. Chinese Science Bulletin, 48(6): 605-610. 66 Li R W,Wan Y S,Cheng Z Y.2005. Provenance of Jurassic sediments in the Hefei Basin,east-central China and the contribution of high-pressure and ultrahigh-pressure metamorphic rocks from the Dabie Shan. Earth and Planetary Science Letters, 231(3-4): 279-294. 67 Li S G,Xiao Y L,Liu D L,Chen Y Z,Ge N J,Zhang Z Q,Sun S S,Cong B,Zhang R,Hart S R,Wang S S.1993. Collision of the North China and Yangtse Blocks and formation of coesite-bearing eclogites: Timing and processes. Chemical Geology, 109(1-4): 89-111. 68 Li S G,Jagoutz E,Xiao Y L,Ge N J,Chen Y Z.1996. Chronology of ultrahigh-pressure metamorphism in the Dabie Mountains and Su-Lu terrane: Ⅰ. Sm-Nd isotope system. Science in China: Series D, 39(6): 597-609. 69 Li S G,Jagoutz E,Chen Y Z,Li Q L.2000. Sm-Nd and Rb-Sr isotopic chronology and cooling history of ultrahigh pressure metamorphic rocks and their country rocks at Shuanghe in the Dabie Mountains,central China. Geochimica et Cosmochimica Acta, 64(6): 1077-1093. 70 Li S G,Huang F,Zhou H Y,Li H M.2003b. U-Pb isotopic compositions of the ultrahigh pressure metamorphic(UHPM)rocks from Shuanghe and gneisses from northern Dabie zone in the Dabie Mountains,central China: Constraint on the exhumation mechanism of UHPM rocks. Science in China: Series D, 46(3): 200-209. 71 Li S Y,Li R W,Meng Q R,Wang D X,Liu Y.2006. Radiometric dating sediments derived from metamorphic rocks of the Dabie orogenic belt in the Jurassic and Early Cretaceous. Progress in Natural Science,16(Special Issue): 194-202. 72 Li Z,Li R W,Sun S,Zhang W H.2001. Rb-Sr chronological characteristics of Jurassic granitoid gravels in the northern margin of the Dabie Block. Chinese Science Bulletin, 46(13): 1126-1129. 73 Liu S F,Zhang G W,Zhang Z Q,Su S G.2001. Isotopic chronological tracer of granite gravel in Hefei Basin. Chinese Science Bulletin, 46(20): 1716-1722. 74 Liu S F,Zhang G W,Bradley D R,Zhang H P,Gao M X,Qian C C.2010. Tracing exhumation of the Dabie Shan ultrahigh-pressure metamorphic complex using the sedimentary record in the Hefei Basin,China. Geological Society of America Bulletin, 122: 198-218. 75 Liu Y,Hu Z,Gao S,Detlef G,Xu J,Gao C.2008. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard. Chemical Geology, 257(1-2): 1-43. 76 Ludwing K R.2003. Isoplot: A Geochronological Toolkit for Microsoft Excel,Special Publication. Berkeley Geochronology Center,1-70. 77 Meng Q R,Li S Y,Li R W.2007. Mesozoic evolution of the Hefei Basin in eastern China: Sedimentary response to deformations in the adjacent Dabieshan and along the Tanlu fault. Geological Society of America Bulletin,119(7/8): 897-916. 78 Neal J M,Rasmussen B,Fletcher I R.1999. SHRIMP uranium-lead dating of diagenetic xenotime in siliciclastic sedimentary rocks. Science, 285: 78-80. 79 Okay A I,Sengör A M C.1992. Evidence for intracontinental thrust-related exhumation of the ultra-high-pressure rocks in China. Geology, 20: 411-414. 80 Okay A I,Şengör A M C,Satir M.1993. Tectonics of an ultrahigh-pressure metamorphic terrane: The Dabie Shan/Tongbai Shan Orogen,China. Tectonics, 12(6): 1320-1334. 81 Pang X,Yang S K,Zhu M.2004. Deep-water fan systems and petroleum resources on the northern slope of the South China Sea. Acta Geologica Sinica, 78(3): 626-631. 82 Pelsmaeker E D,Jolivet M,Laborde A.2017. Source-to-sink dynamics in the Kyrgyz Tien Shan from the Jurassic to the Paleogene: Insights from sedimentological and detrital zircon U-Pb analyses. Gondwana Research, 54: 180-204. 83 Peter R W,Zhou Z Y,Ehlers T A,Xu C H,Brandon M T,Donelick B A,Nicolescu S.2003. Post-orogenic evolution of the Dabie Shan,eastern China,from(U-Th)/He and fission-track thermochronology. American Journal of Science, 303: 489-518. 84 Ratschbacher L,Hacker B R,Webb L E,McWilliams M.2000. Exhumation of the ultrahigh-pressure continental crust in east central China: Cretaceous and Cenozoic unroofing and the Tan-Lu fault. Journal of Geophysical Research-Solid Earth, 105: 13303-13338. 85 Rowley D B,Xue F,Tucker R D,Peng Z X,Baker J,Davis A.1997. Ages of ultrahigh pressure metamorphism and protolith orthogneisses from the eastern Dabie Shan: U/Pb zircon geochronology. Earth and Planetary Science Letters, 151: 191-203. 86 Sláma J,Kosler J,Condon D J,Crowley J L,Gerdes A,Hanchar J M,Horstwood M S A,Morris G A,Nasdala L,Norberg N,Schaltegger U,Schoene B,Tubrett M N,Whitehouse M J.2008. Plesovice zircon: A new natural reference material for U-Pb and Hf isotopic microanalysis. Chemical Geology, 249: 1-35. 87 Schafer J,Dorr W.1997. Heavy-mineral analysis and typology of detrital zircons: A new approach to provenance study(Saxothuringian flysch,Germany). Journal of Sedimentary Research, 67(3): 451-461. 88 Snedden J W,Galloway W E,Milliken K T,Xu J,Whiteaker T,Blum M D.2018. Validation of empirical source-to-sink scaling relationships in a continental-scale system: The Gulf of Mexico basin Cenozoic record. Geosphere, 14(2): 768-784. 89 Tucker R T,Roberts E M,Hu Y,Kemp A I S,Salisbury S W.2013. Detrital zircon age constraints for the Winton Formation,Queensland: Contextualizing Australia's Late Cretaceous dinosaur faunas. Gondwana Research, 24: 767-779. 90 Wang D X,Liu Y,Li S Y,Jin F Q.2002. The time limit of the exhumation of ultrahigh-pressure metamorphic rocks in the Dabie Mountains: The discovery of eclogite gravels in the Late Jurassic conglomerates in the northern Dabie Mountains. Chinese Science Bulletin, 47: 231-235. 91 Wang E Q,Meng Q R,Burchfiel B C,Zhang G W.2003. Mesozoic large-scale lateral extrusion,rotation,and uplift of the Tongbai-Dabie Shan belt in east China. Geology, 31(4): 307-310. 92 Wang X M,Liou J G,Mao H K.1989. Coesite bearing eclogite from the Dabie Mountains in central China. Geology, 17: 1085-1088. 93 Wiedenbeck M,Allé P,Corfu F,Griffin W L,Meier M,Oberli F.1995. Three natural zircon standards for U-Th-Pb,Lu-Hf,trace element and REE analyses. Geostandards Newsletter, 19(1): 1-23. 94 Xue F,Rowley D B,Tucker R D,Zhan X P.1997. U-Pb zircon ages of granitoid rocks in the North Dabie Complex,eastern Dabie Shan,China. The Journal of Geology, 105(6): 744-753. 95 Xu S T,Okay A J,Ji S Y,Sengör A M C,Su W,Liu Y C,Jiang L L.1992. Diamond from the Dabie Shan metamorphic rocks and its implication for tectonic setting. Science, 256: 80-82. 96 Yang W,Jolivet M.2013. Source to sink relations between the Tian Shan and Junggar Basin(northwest China)from Late Paleozoic to Quaternary: Evidence from detrital U-Pb zircon geochronology. Basin Research, 25(2): 219-240. 97 Ye K,Cong B,Ye D.2000. The possible subduction of continental material to depths greater than 200 km. Nature, 407: 734-736. 98 Zhai M G,Cong B L,Zhao Z F,Wang Q C,Wang G,Jiang L L.1995. Petrological-tectonic units in the coesite-bearing metamorphic terrain of the Dabie Mountains,central China and their geotectonic implications. Journal of Southeast Asian Earth Sciences, 1(1): 1-13. 99 Zhang R Y,Liou J G,Ernst W G.2009. The Dabie-Sulu continental collision zone: A comprehensive review. Gondwana Research, 16: 1-26. 100 Zheng Y F,Fu B,Gong B,Xiao Y L,Ge N J.1997. U-Pb dating of marble associated with eclogite from the Dabie Mountains,East China. Acta Geochimica, 16(3): 193-201. 101 Zheng Y F,Fu B,Gong B,Li L.2003. Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China: Implications for geodynamics and fluid regime. Earth-Science Review, 62(1-2): 105-161. 102 Zheng Y F,Zhou J B,Wu Y B,Xie Z.2005. Low-grade metamorphic rocks in the Dabie-Sulu orogenic belt: A passive-margin accretionary wedge deformed during continent subduction. International Geology Review, 47(8): 851-871. 103 Zhou Z Y,Reiners P W,Xu C H,Liao Z T,Yang F L.2002. Zircon(U-Th)/He thermochronological constraints on Cretaceous thermal extension of Dabieshan orogen. Progress in Natural Science, 12: 524-527. 104 Zhu G,Wang Y S,Wang W,Zhang S A,Liu C,Gu C C,Li Y J.2017. An accreted micro-continent in the north of the Dabie Orogen,East China: Evidence from detrital zircon dating. Tectonophysics, 698: 47-64.
