Establishment of the Middle—Upper Triassic Garezhadi Formation in the Coqen Block, Tibet
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摘要:
在西藏措勤断块新建了中三叠统—上三叠统卡尼阶岩石地层单位——嘎热扎地组。在建组剖面上,嘎热扎地组厚约485 m,下部岩性以碎屑岩为主,上部岩性为碎屑岩夹灰岩。嘎热扎地组与下伏上二叠统—下三叠统木纠错组、上覆上三叠统诺利阶麦龙岗组均为整合接触关系。该组尚未发现指示地层时代的化石,但前人在其下伏的木纠错组中发现了早三叠世牙形石,本次在其上覆的麦龙岗组发现7属8种珊瑚化石:Distichophyllia norica(Frech),Retiophyllia? sp.,Gablonzeria? sp.,Elysastraea juliana Turnšek,Volzeiasublaevis(Münster),Distichophyllia sp.,Guembelastraea? sp.和Beneckastraea baiyuensis Deng&Zhang。根据该组地层整合于两者之间,将其时代暂时限定为中—晚三叠世卡尼期。根据珊瑚化石、地层岩性特征及上下地层关系将研究剖面的地层进行了重新划分。嘎热扎地组的建立填补了措勤断块局限台地相三叠系序列中三叠统—上三叠统卡尼阶岩石地层单位名称的空白。嘎热扎地组建立以后,措勤断块局限台地相三叠系的岩石地层单位序列可以划分为上二叠统—下三叠统木纠错组,中三叠统—上三叠统卡尼阶嘎热扎地组,上三叠统诺利阶麦龙岗组,上三叠统瑞替阶—下侏罗统确哈拉组。这一序列的建立对于在措勤断块进一步识别出碳酸盐岩局限台地相三叠系,修订相关地区的地层认识具有指导作用。
Abstract:A new lithostratigraphic unit in the Middle Triassic-Upper Triassic Carnian, the Garezhadi Formation, was established in the Coqen Block, Tibet.In the profile of the newly established lithostratigraphic unit, the Garizadi Formation is about 485 m thick.The lower lithology is dominated by clastic rocks, while the upper lithology is clastic rocks intercalated with limestone.It is conformable with both the overlying Upper Triassic Mailonggang Formation and the underlying Upper Permian-Lower Triassic Mujiucuo Formation.No fossils indicating the stratigraphic age have been found in it, but Early Triassic conodonts have been found in the underlying Mujiucuo Formation by previous work, and in our project, eight coral species belonging to seven genus were identified in the overlying Mailonggang Formation, including Distichophyllia norica (Frech), Retiophyllia? sp., Gablonzeria? sp., Elysastraea juliana Turnšek, Volzeia sublaevis (Münster), Distichophyllia sp., Guembelastraea? sp., Beneckastraea baiyuensis.According to its conformable contact with the underlying and overlying strata, the age of Garezhadi Formation is temporarily limited to the Middle-Triassic Late Triassic Carnian period.Moreover, the stratum observed in the measured profile was reclassified based on the age of corals, lithology and its contact relationships.The establishment of the Garezhadi Formation filled the naming blank of the lithostratigraphic units of the restricted platform facies of Triassic sequence in Coqen block.Its establishment resulted in the Triassic stratigraphic sequence of the restricted platform facies being divided into the Upper Permian-Lower Triassic Mujiucuo Formation, the Middle Triassic—Upper Triassic Carnian Garezhadi Formation, the Upper Triassic Norian Mailonggang Formation, the Upper Triassic Rhaetian-? Lower Jurassic Quehala Formation in asending order.The establishment of this sequence has a guiding role in further identifying the Triassic system of restricted carbonate platform facies and revising the stratigraphic understanding of related areas in Coqen block.
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Key words:
- Tibet /
- Coqen Block /
- Garezhadi Formation /
- Middle—Upper Triassic /
- coral
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图 2 保吉地区地质图[11]
Figure 2.
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[1] 赵政璋, 李永铁, 叶和飞, 等. 青藏高原地层[M]. 北京: 科学出版社, 2001: 1-542.
[2] 潘桂棠, 莫宣学, 侯增谦, 等. 冈底斯造山带的时空结构及演化[J]. 岩石学报, 2006, 22(3): 521-533. https://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200603001.htm
[3] 王剑, 丁俊, 王成善, 等. 青藏高原油气资源战略选区调查与评价[M]. 北京: 地质出版社, 2009.
[4] 纪占胜, 姚建新, 武桂春, 等. 西藏措勤县敌布错地区"下拉组"中发现晚三叠世诺利期高舟牙形石[J]. 地质通报, 2006, 25(1): 138-141. doi: 10.3969/j.issn.1671-2552.2006.01.021
[5] 纪占胜, 姚建新, 武桂春. 西藏冈底斯西段措勤地区海相三叠系的划分[J]. 地质通报, 2007, 26(8): 947-952. doi: 10.3969/j.issn.1671-2552.2007.08.005
[6] 武桂春, 姚建新, 纪占胜. 西藏冈底斯西段措勤地区三叠纪牙形石生物地层特征[J]. 地质通报, 2007, 26(8): 938-946. doi: 10.3969/j.issn.1671-2552.2007.08.004
[7] 纪占胜, 姚建新, 武桂春. 西藏冈底斯南部措勤县鸭洼地区麻木下组时代的修订及其地质意义[J]. 地质学报, 2010, 84(10): 1379-1388. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201010001.htm
[8] 武桂春, 纪占胜, 姚建新. 西藏班戈地区三叠系牙形石生物地层[J]. 地质论评, 2013, 59: 72-73. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-DXHD201304001034.htm
[9] 石秋圆. 西藏保吉地区晚三叠世诺利期地层及其沉积环境[D]. 中国地质大学(北京)硕士学位论文, 2019.
[10] 武桂春, 纪占胜, 姚建新, 等. 纳木错西岸白云岩的时代修订及油浸现象发现的意义[J]. 地质学报, 2017, 91(12): 2867-2880. doi: 10.3969/j.issn.0001-5717.2017.12.020
[11] Wu G C, Ji Z S, Trotter J A, et al. Conodont biostratigraphy of a new Permo-Triassic boundary section at Wenbudangsang, north Tibet[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2014, 411: 188-207. doi: 10.1016/j.palaeo.2014.06.016
[12] 纪占胜, 姚建新, 武桂春. 西藏西部狮泉河地区二叠纪和三叠纪牙形石的发现及其意义[J]. 地质通报, 2007, 26(4): 383-397. doi: 10.3969/j.issn.1671-2552.2007.04.003
[13] 郑有业, 许荣科, 王成源, 等. 冈底斯西缘早三叠世牙形石的发现及淌那勒组的建立[J]. 中国科学(D辑), 2007, 37(7): 916-921. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200707006.htm
[14] 孟亚洲, 纪占胜, 廖卫华, 等. 西藏保吉地区晚侏罗世动物群的发现及其意义[J]. 地质学报, 2016, 90(5): 833-847. doi: 10.3969/j.issn.0001-5717.2016.05.001
[15] 孙倩, 纪占胜, 武桂春, 等. 西藏措勤盆地上侏罗统吐卡日组上下段的厘定及其礁灰岩发现的油气勘探意义[J]. 地球学报, 2018, 39(4): 419-431. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201804005.htm
[16] 孙倩, 纪占胜, 武桂春, 等. 西藏措勤盆地上侏罗统萨波直不勒组的发现及其烃源岩[J]. 地球学报, 2018, 39(4): 432-444. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201804006.htm
[17] 廖卫华, 纪占胜, 武桂春. 西藏改则的晚侏罗世石珊瑚[J]. 古生物学报, 2012, 51(3): 290-307. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX201203004.htm
[18] 赵兵, 刘登忠, 陶晓风, 等. 西藏措勤-申扎地层分区新建中-上侏罗统仁多组[J]. 地质通报, 2005, 24(7): 637-641. doi: 10.3969/j.issn.1671-2552.2005.07.008
[19] 纪占胜, 姚建新, 武桂春. 西藏改则县物玛乡北部晚侏罗世吐卡日组珊瑚动物群的发现及其地质意义[J]. 地质通报, 2011, 30(2/3): 418-438. http://dzhtb.cgs.cn/gbc/ch/reader/view_abstract.aspx?file_no=2011020329&flag=1
[20] 纪占胜, 姚建新, 武桂春. 关于藏北改则地区夏岗江植物群及其地层时代的修订意见[J]. 地质通报, 2007, 26(8): 953-959. doi: 10.3969/j.issn.1671-2552.2007.08.006
[21] 李晓勇, 谢国刚, 徐银保, 等. 西藏中南部尼雄-文部地区中-晚二叠世坚扎弄组的发现及其地质意义[J]. 地质通报, 2002, 21(6): 339-344. doi: 10.3969/j.issn.1671-2552.2002.06.010
[22] 周幼云, 江元生, 王明光. 西藏措勤-申扎地层分区二叠系敌布错组的建立及其特征[J]. 地质通报, 2002, 21(2): 79-82. doi: 10.3969/j.issn.1671-2552.2002.02.006
[23] 程立人, 王天武, 李才, 等. 藏北申扎地区上二叠统木纠错组的建立及皱纹珊瑚组合[J]. 地质通报, 2002, 21(3): 140-143. doi: 10.3969/j.issn.1671-2552.2002.03.006
[24] 纪占胜, 武桂春, 姚建新, 等. 青藏高原油气勘探战略选区和战术突破目标的建议[J]. 地球学报, 2018, 39(4): 387-400. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201804002.htm
[25] 何继富, 纪占胜, 武桂春, 等. 西藏措勤盆地保吉地区上二叠统-下三叠统木纠错组显微荧光特征及油气勘探建议[J]. 地球学报, 2018, 39(4): 463-473. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201804009.htm
[26] 纪占胜, 姚建新, 武桂春. 西藏措勤盆地的上古生界-下中生界: 潜在的油气沉积建造[J]. 地质通报, 2008, 27(1): 36-63. doi: 10.3969/j.issn.1671-2552.2008.01.004
[27] 纪占胜, 姚建新, 武桂春, 等. 西藏措勤盆地的地层学研究进展及上二叠统-侏罗系地层序列的厘定[J]. 地球学报, 2018, 39(4): 401-407. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201804003.htm
[28] 纪占胜, 姚建新, 武桂春. 藏北羌塘中央隆起带果干加年山晚三叠世珊瑚化石发现及其地质意义[J]. 地质学报, 2010, 84(8): 1095-1104. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201008003.htm
[29] 仲昭, 纪占胜, 武桂春, 等. 西藏班戈县保吉乡纳木错西下石炭统珊瑚动物群的发现及其意义[J]. 地质论评, 2017, 63(S1): 333-334. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2017S1161.htm
[30] Bo J F, Wang X L, Gao J H, et al. Upper Triassic reef coral fauna in the Renacuo area, northern Tibet, and itsimplications for palaeobiogeography[J]. Journal of Asian Earth Sciences, 2017, 146: 114-133. doi: 10.1016/j.jseaes.2017.05.006
[31] 王乃文. 藏北湖区中生代地层发育及其板块构造含义[C]//李廷栋. 青藏高原地质文集(8)-地层古生物. 1983: 34-35.
[32] 陈楚震, 王玉净. 拉萨-波密分区. [C]//西藏地层. 北京: 科学出版社, 1984, 141-147.
[33] 饶荣标, 徐济凡, 陈永明, 等. 青藏高原的三叠系[M]. 北京: 地质出版社, 1987.
[34] 石秋圆, 纪占胜, 武桂春, 等. 西藏格仁错北沿岸中二叠世珊瑚化石的发现[J]. 地质论评, 2017, 63(S1): 319-320. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP2017S1155.htm
[35] 石秋圆, 纪占胜, 武桂春, 等. 西藏申扎县格仁错北岸中上泥盆统查果罗玛组中发现中晚二叠世珊瑚化石[J]. 地球学报, 2018, 39(4): 453-462. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB201804008.htm
① 中国地质科学院地质力学研究所. 中华人民共和国1: 25万区域地质调查报告(当雄县幅). 2003.