新疆库鲁克塔格地区新元古代层序地层学研究及对比
Neoproterozoic sequence stratigraphy and correlation in Quruqtagh area, Xinjiang
-
摘要: 新疆库鲁克塔格地区上元古界可分为五个沉积层序，由下到上分别对应于贝义西组、照壁山组、阿勒通沟组、特瑞爱肯组至水泉组和汉格尔乔克组。第1层序由贝义西组构成，发育由粗碎屑斜坡扇和低水位楔构成的低水位体系域，向上逐渐变为粉砂岩、泥岩的海进体系域，并以向上变粗的退积准层序的高水位体系域结束，反映陆缘发展初期海平面的升降变化。第2层序由照壁山组构成，底部为粗粒石英砂岩，向上变为细粒砂岩、页岩互层，上部出现厚约30m的泥岩，顶部为紫红色砂岩，代表了由低水位经快速海进到高水位的变化过程，整体为水体较浅的滨浅海沉积环境。第3层序由阿勒通沟组构成，为冰成杂砾岩、砂岩、页岩组合，顶部出现厚2～3m的白云岩，沉积主体为低水位体系域，顶部白云岩为海进体系域，缺失高水位体系域。第4层序发育最为完整，特瑞爱肯组冰成杂砾岩为低水位体系域，冰成杂砾岩之上“盖帽碳酸盐岩”为海进体系域，扎摩克提组浊积岩、育肯沟组页岩、水泉组碳酸盐岩为高水位体系域，其中育肯沟组页岩为凝缩段沉积。第5层序低水位体系域由汉格尔乔克组冰成杂砾岩构成，顶部泥灰岩和白云岩为海进体系域，由于顶部被寒武系不整合覆盖，缺失高水位体系域。研究区上元古界层序基本可以和我国华南及印度Lesser Himalaya地区对比。
-
Key words:
- Sequence stratigraphy /
- Neoproterozoic /
- Quruqtagh area /
- Xinjiang
-
-
[1] 储雪蕾.2004.新元古代的"雪球地球".矿物岩石地球化学通报,23(3):233-238
[2] Beyth M,Avigad D,Wetzel H U,Matthews A and Berhe SM.2003. Crustal exhumation and indications for Snowball Earth in the East African Orogen:north Ethiopia and east Eritrea.Precambrian Research,123:187 -201
[3] Christie-Blick N,Dyson lA and Borch CC.1995. Sequence stratigraphy and the interpretation of Neoprotorozoic earth history.Precambrian Research,73:3-26
[4] 储雪蕾,Wolfgang Todt,张启锐,陈福坤,黄晶.2005.南华-震旦系界线的锆石U-Pb年龄.科学通报,50(6):600-603
[5] Chu XL.2004. Snowball Earth during the Neoproterozoic.Bulletin of Mineralogy,Petrology and Geochemistry,23 (3):233-238 (in Chinese)
[6] 高长林,叶德燎,黄泽光.2004.塔里木库鲁克塔格古原洋裂谷与地幔柱.石油实验地质,26(2):161-168
[7] 高振家,朱诚顺.1984.新疆前寒武纪地质.乌鲁木齐:新疆人民出版社,1-151
[8] Chu XL,Todt W,Zhang QR,Chen FK and Huang J.2005. U-Pb Zircon Age of the Nanhua-Sinian Boundary.Chinese Science Bulletin,50(6):600-603(in Chinese)
[9] Daniel C,Zhu MY,Bowring S,Wang W,Yang AH and Jin YG.2005. U-Pb Ages from the Neoproterozoic Doushantuo Formation,China.Science,308:95 -98
[10] 高振家,陈克强.2003.新疆的南华系及我国南华系的几个地质问题.地质调查与研究,26(1):8-14
[11] Gao CL,Ye DL and Huang ZG.2004. Kuruktag Ur-ocean rift and Mantle plume in the Tarim Basin.Petroleum Geology and Experiment,26 (2):161-168 (in Chinese)
[12] 姜常义,白开寅,黑爱芝,赵晓宁,张虹波.2000.库鲁克塔格地区火山岩的岩浆过程与源区组成.岩石矿物学杂志,19(1):8-18
[13] Gao ZJ and Chen KQ.2003. The Nanhua Syetem of Xinjiang and some Geological Issues of Nanhua system in China.Geological Survey and Research,26(1):8-14(in Chinese)
[14] 李怀坤,董玉杰.1991.新疆中库鲁克塔格地区震旦系扎摩克提组沉积特征.新疆地质,9(4):340-353
[15] 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):304-317
[16] Gao ZJ and Zhu CS.1984. Precambrian Geology in Xinjiang,China.Urumqi:Xinjiang People Press.pp1-151.(in Chinese)
[17] 李秋根,刘树文,韩宝福,郭召杰,张志诚,郑海飞,杨斌.2004.新疆库鲁克塔格震旦系冰碛岩的地球化学特征及其对物源区的指示.自然科学进展,14(9):999-1005
[18] Germs GJB.1995. The Neoproterozoic of southwestern Africa,with emphasis on platform stratigraphy and paleontology.Precambrian Research,73:137-151
[19] 陆松年,李怀坤,陈志宏,于海峰,金巍,郭坤一.2004.新元古时期中国古大陆与罗迪尼亚超大陆的关系.地学前缘(中国地质大学,北京),11(2):515-523
[20] Hoffman PF,Kaufman AJ,Halverson GP and Schrag DP.1998. A Neoproterozoic Snowball Earth.Science,28:1342-1344
[21] Hoffman PF and Schrag DP.2002. The snowball earth hypothesis:testing the limits of the global change.Terra Nova,14(3):129-155
[22] 王剑.2000.华南新元古代裂谷盆地演化-兼论与Rodinia解体的关系.北京:地质出版社.1-146.
[23] Jiang CY,Bai KY,Hei AZ,Zhao XN and Zhang HB.2000. Petrology,Geochemistry,Magmatic process and Source Composition of SinianCambrian Volcanic Rocks in Kuruktag Area.Acta Petrologica et Mineralogica,19 (1):8-18 (in Chinese)
[24] 王剑.2001.华南新元古代裂谷盆地演化-Rodinia超大陆解体的前奏.矿物岩石,21(3):135-145
[25] 尹崇玉.2005.国际新元古代年代地层学研究进展与发展趋势.地层学杂志,29(2):178-179,214
[26] Jiang GQ,Wang ZQ and Zhang LH.1996. Sequence Stratigraphy of Upper Proterozoic Glacigenous Rocks in Southeastern Margin of Yangtze Platform.Journal of China University of Geosciences,7 (1):38-45(in Chinese with English abstract)
[27] Jiang GQ,Christie-Blick N,Kaufman AJ,Banerjee DM and Raj V.2002. Sequence stratigraphy of the Neoproterozoic Infra Krol Formation and Krol Group,Lesser Himalaya,India.Journal of Sedimentary Research,72(4):524 -542
[28] 张启锐,储雪蕾.2006.扬子地区江口冰期地层的划分对比与南华系层型剖面.地层学杂志,30(4):306-314
[29] Jiang GQ,Christie-Blick N,Kaufman AJ,Banerjee DM and Rai V.2003. Carbonate platform growth and cyclicity at a terminal Proterozoic passive margin,infra Krol Formation and Krol Group,Lesser Himalaya,India.Sedimentology,50:921-952
[30] Jiang GQ,Kennedy MJ and Christie-Blick N.2003a.Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates.Nature,426:822-826
[31] Jiang GQ,Sohl LE and Christie-Blick N.2003. Neoproterozoic stratigraphic comparison of the Lesser Himalaya(India) and Yangtze Block (South China):paleogeographic implications.Geology,31:917-920
[32] Jiang GQ,Kennedy MJ,Christie-Blick N,Wu H and Zhang S.2006. Stratigraphy,sedimentary structures,and textures of the late Neoproterozoic Doushantuo cap carbonate in south China.Journal of Sedimentary Research,76:978-995
[33] Kaufman AJ,Jiang GQ,Christie-Blick N,Banerjee DM and Rai V.2006. Stable isotope record of the terminal Neoproterozoic Krol platform in the Lesser Himalayas of northern India.Precambrian Research,147:156-185
[34] Kennedy MJ,Runnegar B,Pave AR,Hoffman KH and Arthur MA.1998. Two or four Neoproterozoic glaciations? Geology,26:1059-1063
[35] Kilner B,Niocaill CM and Brasier M.2005. Low-latitude glaciation in the Neoproterozoic of Oman.Geology,33(5):413 -416
[36] Knoll AH.2000. Learning to toll Neopeoterozoic time.Precambrian Research,100:3-20
[37] Li HK and Dong YJ.1991. Sedimentary features of Sinian Zhamoketi Formation in the Middle Kuruktag Area,Xinjiang.Xinjiang Geology,9(4):340-353(in Chinese)
[38] Li JT.2004. Late Neoproterozoic and Paleozoic Tectonic Framework and Evolution of Eastern Xinjiang,NW China.Geological Review,50(3):304 -317(in Chinese)
[39] Lu SN,Li HK,Chen ZH,Yu HF,Jin W and Guo KY.2004. Relationship Between Neoproterozoic Cratons of China and Rodinia.Earth Science Frontiers(China University of Geosciences,Beijing),11(2):515 -523(in Chinese)
[40] Ma G,Lee H and Zhang Z.1984. An investigation of the age limits of the Sinian System in south China.Chinese Academia of Geological Sciences,Bulletin of Yichang Institute of Geology and Mineral Resource,8:1-29 (in Chinese)
[41] Pyle LJ,Narbonne GM,James NP,et al.2004. Integrated Ediacaran chronostratigraphy,Wernecke Mountains,northwestern Canada.Precambrian Research,132:1-27
[42] Stern RJ,Avigad D,Miller NR and Beyth M.2006. Evidence for the Snowball Earth hypothesis in the Arabian-Nubian Shield and the East African Orogen.Journal of African Earth Sciences,44:1 -20
[43] Torsvik TH,Carter LM,Ashwal LD,Bhushan MK,Pandit and Jamtveit B.2001. Rodinia refined or obscured:Palaeomagnetism of the Malani igneous suite (northwest India).Precambrian Research,108:319 -333
[44] Walter MR,Veevers CR and Grey CK.1995. Neoproterozoic stratigraphy of the Centralian Superbasin,Australia.Precambrian Research,73:173-195
[45] Wang J.2000. Neoproterozoic Rifting History of South China:Significance to Rodinia Breakup.Beijing:Geological Press.pp1-146.(in Chinese)
[46] Wang J,Liu BJ and Pan GT.2001. Neoproterozoic Rifting History of South China Significance to Rodinia Breakup.Journal of Mineralogy and Petrology,21 (3):135-145(in Chinese)
[47] Wang ZQ,Gao LZ,Zhang LH,Jiang GQ,Zhang CH and Yin Y.1996. Sequence Stratigraphy and Relative Sea Level Changes in Sinian System of Yichang,Hubei Province.Journal of China University of Geosciences,7(1):29 -37
[48] Xiao SH,Bao HM,Wang HF,Kaufman AJ,Zhou CM,Li G X,Yuan XL and Ling HF.2004. The Neoproterozoic Quruqtagh Group in eastern Chinese Tianshan:evidence for a post-Marinoan glaciation.Precambrian Research,130:1-26
[49] Xu B,Zheng HF,Yao HT and Li YA.2003. C-isotope composition and significance of the Sinian on the Tarim plate.Chinese Science Bulletin,48(4):385 -389
[50] Xu B,Jian P,Zheng HF,Zhou HB,Zhang LF and Liu DY.2005. U-Pb zircon geochronology and geochemistry of Neoproterzoic volcanic rocks in the Tarim Block of northwest China:implications for the breakup of Rodinia supercontinent and Neoproterozoic glaciations.Precambrian Research,136:107-123
[51] Yin CY.2005. Advance and Tendency of the Neoproterozoic Chronostratigraphic Studies.Journal of Stratigraphy,29 (2):178-179,214(in Chinese)
[52] Zhang QR and Chu XL.2006. The Stratigraphic Classification and Correlation of the J iangkou Glaciation in the Yangtze Block and the Stratotype Section of the Nanhuan system.Journal of Stratigraphy,30(4):306-314(in Chinese)
[53] Zhou CM,Tucker RS,Xiao SH,Peng ZX,Yuan XL and Chen Z.2004. New constraints on the ages of Neoproterozoic Glaciations in south China.Geology,32:437-440
-
计量
- 文章访问数: 6814
- PDF下载数: 8988
- 施引文献: 0
下载: