全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...
地质学报  2005 

大别造山带北缘古生代构造-地层岩片沉积物源区及构造演化的地球化学研究

, PP. 402-413

Keywords: 碎屑岩,构造-地层岩片,沉积物源区,成分成熟度,地球化学,北淮阳

Full-Text   Cite this paper   Add to My Lib

Abstract:

取自大别造山带北缘(北淮阳地区)古生代主要构造-地层岩片中变碎屑岩和碎屑岩的一组元素和Nd同位素地球化学数据与相关资料显示,从早古生代到泥盆纪,再到石炭纪,龟山组、南湾组―佛子岭群和石炭系三个岩片中的碎屑岩类,存在稳定的沉积物源区,源区组成可能相当于北秦岭构造单元中古元古代的秦岭群及秦岭群组分沉积再循环的部分。沉积组分成熟度由高到低和源区剥蚀性质变化的地球化学记录,指示三个岩片代表了华北、扬子两陆块在古生代构造演化过程中,主动大陆边缘一侧一系列构造事件中“俯冲后期-对接-碰撞前奏”的三个片断。这些论证显示,大别造山带北缘不同岩片沉积构造环境和演化的进程完全可以与北秦岭构造单元南部对比,大别造山带北缘应是北秦岭构造单元的东延部分。

References

[1]  刘景波.[D].中国地质大学,1994.
[2]  陈廷愚 牛宝贵.大别山腹地燕山期岩浆作用和变质作用的同位素...[J].地质学报,:.
[3]  戴圣潜 徐家聪.北淮阳东段佛子岭群新认识[J].中国区域地质,:.
[4]  高山 张本仁.华北与杨子板块志留―泥盆纪对接的沉积地球化学证据[J].中国科学:B辑,:.
[5]  胡圣虹 陈爱芳 林守麟.地质样品中40个微量、痕量、超痕量元素的ICP―MS分析研究[J].地球科学,2000,25:186~190.
[6]  凌文黎.扬子克拉通黄陵地区崆岭杂岩Sm―Nd同位素地质年代学研究[J].科学通报,:.
[7]  凌文黎 高山.扬子陆核古元古代晚期构造热事件与扬子克拉通演化[J].科学通报,:.
[8]  刘少峰 张国伟.东秦岭―大别山及邻区挠曲类盆地演化与碰撞造山过程[J].地质科学,:.
[9]  刘文灿 王果胜.北淮阳地区中生代逆冲推覆构造[J].现代地质,:.
[10]  索书田 钟增球.大别―苏鲁构造带三叠纪碰撞缝合线的位置[J].地球科学:中国地质大学学报,:.
[11]  吴维平.大别山东部桐城挂镇地区超高压变质杂岩的变形历史[J].安徽地质,2000,10:199.
[12]  徐树侗 江来利.大别山区(安徽部分)的构造格局和演化过程[J].地质学报,:.
[13]  徐树桐 刘贻灿 等.大别山造山带研究的主要进展及存在的问题[J].自然科学进展:国家重点实验室通讯,:.
[14]  杨坤光 马昌前.北淮阳马畈加里东岩体的研究及其地质意义[J].地球科学:中国地质大学学报,:.
[15]  张宗清 刘敦一 等.北秦岭变质地层同位素年代学研究[M].北京:地质出版社,1994.199.
[16]  Bhatia M R.1985. REE geochemistry of Australian Paleozoic graywackes and mudrocks: provenance and tectonic control. Sed. Geol. , 45: 97-113.
[17]  Chen T Y, Niu B G, Liu Z G, et al. 1991. Geochronology of Yanshanian magmatism and metamorphism in the hinterland of the Dabie mountains and their geologic significance. Acta Geologica Sinica, 65(4): 329-336 (in Chinese with English abstract).
[18]  Cong B L, Wang Q C. 1999. Recent development in study of Dabie-Sulu UHP rocks. Chinese Science Bulletin, 44:1127-1141 (in Chinese).
[19]  Dai S Q, Xu J C, Shi Q H, et al. 1992. New recognition of the Foziling Group in the eastern part of Northern Huaiyang. Regional Geology of China, (4): 369 -375 (in Chinese with English abstract).
[20]  Gao L D, Liu Z G. 1988. New discovery of microfossils from the Nanwan Formation of the Xinyang Group, Herren and its geological significance. Geological Review, 34 (5): 421 (in Chinese with English abstract).
[21]  Gao S, Zhang B R, Gu X M, et al. 1991. Silurian-Devonian coupling of the north China and Yangtze plates: evidence from the geochemistry of sedimentary rocks. Science in China (series B), 34:1372-1380.
[22]  Li S G, Liu D L, Chen Y Z, et al. 1994. Nd isotopic compositions of continental crust in the northern margin of Yangtze block and its tectonic implications. Geochimica, 23 (supp.): 10- 17 (in Chinese with English abstract).
[23]  Li S G, Han W L, Huang F, et al. 1998. Sm-Nd and Rb-Sr ages geochemistry of volcanics from the Dingyuan Formation in Dabie Mountains, central China: evidence to the Paleozoic magmatic arc. Scientia Geologica Sinica, 7: 461-470.
[24]  Ling W L, Gao S, Zhen H F, et al. 1998. An Sm-Nd isotopic dating study of the Archean Kongling complex in Huangling area of the Yangtze Craton. Chinese Science Bulletin, 43: 1187-1190.
[25]  Liu Z G, Niu B G, Ren J S. 1992. Disintegration of the Xinyang Group and its tectonic implication. Geological Review, 38 (4):293-301 (in Chinese with English abstract).
[26]  Mezger J E, Creaser R A. Erdmer P, et al. 2001. A Cretaceous back-arc basin in the coast belt of the northern Canadian Cordillera,evidence from geochemical and neodymium isotope characteristics of the Kluane metamorphic assemblage, southwest Yukon. Can. J. Earth Sci. , 38: 91-103.
[27]  Okay A I, Sengor A M C, Stair M. 1993. Tectonics of an ultrahigh-pressure metamorphic terrene: the Dabie Shan/Tongbai Shanorogen, China. Tectonics, 12:1320-1334.
[28]  Suo S T, Zhong Z Q, You Z D. 2000. Location of Triassic tectonic suture line between collided Sino-Korean and Yangtze cratons in Dabie--Sulu tectonic zone. Earth Sciences, 25: 111- 116 (in Chinese).
[29]  Wang R N, Wang D, Ouyang S. 1994. New knowledge of the Carboniferous systems in the northern slope of the Dabie Mountains. Journal of Stratigraphy, 18 (1): 17-23(in Chinese).
[30]  Wu W P, Xu S T, Jiang L L, et al. 2000. Deformation history of the UHPM complex in the Guazhen area, Tongcheng, eastern Dabie Mountains. Geology of Anhui, 10:199-204 (in Chinese).
[31]  Xu B, Wang C Q. 2000. Tectonic units in the western Dabie orogenic belts. Geological Journal of China Universities, 6:389-395 (in Chinese with English abstract).
[32]  Xu Q D, Ouyang J P, Zhang B R, et al. 2002. Tectonic affinity of Paleozoic stratigraphic slices along the northern margin in Dabie Orogen,central China: evidence from Pb isotope of rocks.Progress in Natural Science(English edition), 12: 438-444.
[33]  Xu S T, Jiang L L,Liu Y C,et al. 1992. Tectonic framework and -evolution of the Dabie Mountains in Anhui, Eastern China. Acta Geologica Sinica, 66(1):1 - 14 (in Chinese with English abstract).
[34]  Ye B D, Jian P, Xu J W, et al. 1993. The Sujiahe Terrene Collage Belt and Its Constitution and Evolution along the North Hillslope of the Tongbai-Dabie Orogenic Belt. Wuhan: Press of China University of Geoseienees, 5-54 (in Chinese).
[35]  Zhang G W, Meng Q R, Yu Z P, et al.1996. Orogenesis and dynamics of the Qinling Orogen. Science in China (Ser. D), 26 :193-200 (in Chinese).
[36]  Zhang Z Q, Liu D Y, Fu G M. 1994. Isotopic Dating of Metamorphic Stratigraphy in North Qinling Area. Beijing: Geological Publishing House, 1-119 (in Chinese).
[37]  Liu S F, Zhang G W, Cheng S Y, et al. 1999. Evolution of flexural basin and process of collision orogeny in east Qinling-Dabie Shan and its adjacent regions. Scientia Geologica Sinica, 34:336-346(in Chinese with English abstract).
[38]  从柏林 王清晨.大别山―苏鲁超高压变质带研究的最新进展[J].科学通报,:.
[39]  高联达.河南信阳群南湾组微体化石的发现及其地质意义[J].地质论评,1988,36:421-428.
[40]  郝杰 刘小汉.桐柏―大别碰撞造山带大型推覆―滑脱构造及其演化[J].地质科学,1988,(1):1-10.
[41]  李曙光 刘德良 陈移之 张宗清.扬子陆块北缘地壳的钕同位素组成及其构造意义[J].地球化学,1994,23(增刊):10~17.
[42]  刘志刚 牛宝贵.信阳群的解体及其大地构造意义[J].地质论评,:.
[43]  马文璞.大别山北麓有石炭系及其大地构造意义[J].地质学报,:.
[44]  牛宝贵 富云莲 刘志刚.桐柏―大别山主要构造热事件及^40Ar/^39A,地质定年研究[J].地球学报,1994,68(1):20-34.
[45]  王仁农 王怿.大别山北麓石炭系研究新进展[J].地层学杂志,:.
[46]  徐备 王长秋.大别造山带西段构造单元[J].高校地质学报,:.
[47]  徐启东 欧阳建平 等.大别造山带北缘古生代构造―地层岩片的构造归属―岩石铅同位素组成提供的信息[J].自然科学进展,2002,12(5):509-514.
[48]  叶伯丹 简平.桐柏-大别造山带北坡苏家河地体拼接带及其构成和演化[M].武汉:中国地质大学出版社,1993.1-76.
[49]  张本仁 张宏飞 赵志丹.东秦岭及邻区壳、幔地球化学分区和演化及其大地构造意义[J].中国科学(D),1996,26:201-208.
[50]  张国伟 孟庆任.秦岭造山带的造山过程及其动力学特征[J].中国科学:D辑,:.
[51]  Bhatia M R, Crook K A W. 1986. Trace element characteristics of greywackes and tectonic setting discrimination of sedimentary basins. Contrib. Mineral Petrol. , 92 : 181- 193.
[52]  Condie K C, Wilks M, Rosen D M, et al.1991. Geochmistry of metasediments from the Precambrian Hapschan Series, eastern Anabar Shield, Siberia. Precambrian Res., 50: 37-47.
[53]  Creaser R A, Erdmer P. 1997. Tectonic affinity of Nisutlin and Anvil assemblage strata from the Teslin tectonic zone, northern Canadian Cordillera: constraints from neodymium isotope and geochemical evidence. Tectonics, 16:107-121.
[54]  Farmer G L, Ball T T. 1997. Sources of Middle Proterozoic to Early Cambrian siliciclastic sedimentary rocks in the Great Basin: a Nd isotope study. GSA Bulletin, 109: 1193-1205.
[55]  Feng R, Kerrich R, Maas R. 1993. Geochemical,oxygen, and neodymium isotope compositions of metasediments from the Abitibi greenstone belt and Pontiac Subprovince, Canada: Evidence for ancient crust and Archean terrane juxtapodition. Geochim. Cosmochim. Acta, 57.-641-658.
[56]  Hao J, Liu X H. 1988. The large thrust-decollement structure and its evolution of Tongbai-Dabie collision type orogenic belt. Scientia Geologica Sinica, (1) : 1-10 (in Chinese with English abstract).
[57]  Hu S H, Chen A F, Lin S L, et al. 2000. ICP-MS analytical research into 40 trace and ultra-trace elements in geological samples. Earth Sciences, 25:186-190 (in Chinese with English abstract).
[58]  Ling W L, Gao S, Zhang B R, et al. 2000. The recognizing of ca. 1.95 Ga tectono-thermal event in Kongling nuelea and its significance for the evolution of Yangtze Block, south China. Chinese Science Bulletin, 46:26-329.
[59]  Liu W C, Wang G S. 1999. Mesozoic thrust and nappe tectonics in Northern Huaiyang region. Geosciences, 13: 143 - 149 (in Chinese).
[60]  Ma W P. 1991. The Carboniferous at the northern foot of the Dabie mountains and its tectonic implications. Acta Geologica Sinica, 65(1): 17-26 (in Chinese with English abstract).
[61]  McLennan S M, Taylor S R, McCulloch M T, et al. 1990. Geochemical and Nd-Sr isotopic composition of deep-sea turbidites:crustal evolution and plate tectonic associations. Geochim. Cosmochim. Acta, 54:2015-2050.
[62]  Niu B G, Fu Y L, Liu Z G. 1994. Main tectonothermal events and ^40Ar/^39Ar dating of the Tongbai-Dabie Mountains.Acta Geoscientia Sinica,68:20~34(in Chinese with English abstract).
[63]  Patchett P J, Roth M A, Canale B S, et al. 1999. Nd isotopes, geochemistry, and constraints on sources of sediments in the Franklinian mobile belt, Arctic Canada. GSA Bulletin, 111:578-589.
[64]  Roser B P, Korseh R J. 1986. Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio. J. Geol. , 94- 635-650.
[65]  Taylor S R, McLennan S M. 1985. The continental crust:Its composition and evolution. Cambridge: Blackwell.
[66]  Wimmenauer W. 1984. Das pravariskisehe Kristallin im Schwarzwald.Fortsehr. Miner. , 62: 69-86.
[67]  Xu S T, Liu Y S, Wu W P, et al. 2001. The major advance and problem of research in the Dabie orogenic belts. Progress in Natural Sciences, 11:796-803 (in Chinese).
[68]  Yang K G, Ma C Q, Yang W R. 1998. Significance of study of Mafan Caledonian intrusion in Beihuaiyang depression.Earth Sciences, 23:236-241 (in Chinese).
[69]  Zhang B R, Zhang H F, Zhao Z D, et al. 1996. Geochemical subdivision and evolution of the lithosphere in East Qinling and adjacent regions: Implications for tectonics. Science in China (Ser. D), 26:201-208 (in Chinese).

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133