Citation: | YANG Yongfeng, JIANG Yaguo, WANG Tianci, YANG Chunhui, LI Fanglin, TANG Jing. 2016: Petrogeochemistry and sedimentary environment of the Early Cretaceous strata from the Shiquanhe-Gegyai area in Tibet and their geological significance. Geological Bulletin of China, 35(9): 1456-1462. |
Through comprehensive analysis of Early Cretaceous volcanic petrogeochemistry, sedimentary sequence, sedimentary characteristics and environment in the Shiquanhe-Gegyai area, the calc-alkaline volcanic rocks of the Wumulongqianbo Formation may represent plate subduction. The Duoai Formation, Tuocheng Formation and Langjiu Formation make up three partial melting series, indicating presence of arc crust thickening process under the condition of steepened subduction angle. The alkaline volcanic rock of the Langjiu Formation indicates subduction-induced arc crack. The sediments of the Jiega Formation and the Langshan Formation show the same residual basin under the transgression condition after closure of the Shiquanhe ophiolite mélange. The depth of the residual basin is deep in the south and shallow in the north, and deep in the east and shallow in the west. At the same time, angular unconformity occurred at the edge of the basin, which gradually evolved into weak angular unconformity-conformity towards the interior of the basin.
潘桂裳, 李兴振, 王立全, 等.青藏高原及邻区大地构造单元初步划分[J].地质通报, 2002, 21(11):701-707. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=2002011160&journal_id=gbc
|
潘桂棠、丁俊、王立全, 等. 1:150万青藏高原及邻区地质图(附说明书)[M].成都:成都地图出版社, 2010:1-288.
|
潘桂堂、王立全、张万平, 等.青藏高原及邻区大地构造图及说明书(1:150万)[M].北京:地质出版社, 2013:1-208.
|
徐梦婧.青藏高原狮泉河-永珠-嘉黎蛇绿混杂岩带的构造演化[D].吉林大学博士学位论文, 2014:1-150. http://cdmd.cnki.com.cn/article/cdmd-10183-1014267909.htm
|
胡承祖.狮泉河-古昌-永珠蛇绿岩带特征及其地质意义[J].成都理工大学学报(自然科学版), 1990, 1:23-30. http://www.cqvip.com/qk/91405x/199001/5362605.html
|
郑有业, 许荣科, 何来信, 等.西藏狮泉河蛇绿混杂岩带——一个新的多岛弧盆系统的厘定及意义[J].沉积与特提斯地质, 2004, 24(1):13-20. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD200401001.htm
|
康志强, 许继峰, 董彦辉, 等.拉萨地块中北部白垩纪则弄群火山岩:Slainajap洋南向俯冲的产物?[J].岩石学报, 2008, 24(2):303-314. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200802012.htm
|
杨式溥, 宋志敏, 梁定益.西藏阿里(狮泉河-多玛)地区中侏罗-早白垩世复理石相遗迹化石[J].地质学报, 1982, 4:302-313. http://www.cnki.com.cn/article/cjfdtotal-dzxe198204001.htm
|
杨遵仪, 聂泽同, 吴顺宝, 等.西藏阿里地区白垩纪固着蛤类及其地质意义[J].地质学报, 1982, 4:293-301. http://www.cnki.com.cn/Article/CJFDTOTAL-DZXE198204000.htm
|
万晓樵, 吴雁华, 李国彪.西藏白垩纪中期Orbitolinids(有孔虫)的分布与古地理意义[J].地质学报, 2003, 77(1):1-8. http://mall.cnki.net/magazine/article/dzxe200301000.htm
|
潘桂堂, 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. http://www.cnki.com.cn/Article/CJFDTOTAL-YSXB200603001.htm
|
朱弟成, 潘桂堂, 王立全, 等.西藏冈底斯带中生代岩浆岩的时空分布和相关问题的讨论[J].地质通报, 2008, 27(9):1535-1550. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20080913&journal_id=gbc
|
曲晓明, 辛洪波, 杜德道, 等.西藏班公湖-怒江缝合带中段A-型花岗岩的岩浆源区与板片断离[J].地质学报, 2013, 87(6):759-772. http://mall.cnki.net/magazine/article/dzxe201306002.htm
|
李祥辉, 曾庆高, 吴铬, 等.西藏措勤盆地北部下白垩统层序地层特征[J].成都理工大学学报(自然科学版), 2005, 32(2):111-119. http://www.cnki.com.cn/Article/CJFDTOTAL-CDLG200502000.htm
|
谢国刚, 莫宣学, 赵志丹, 等.西藏班公湖地区侏罗纪-白垩纪沉积及古海洋盆地的演化[J].地学前缘, 2009, 4:31-39. http://www.doc88.com/p-874811860202.html
|
朱弟成, 潘桂堂, 莫宣学, 等.冈底斯中北部晚侏罗世-早白垩世地球动力学环境:火山岩约束[J].岩石学报, 2006, 22(3):534-546. http://www.cnki.com.cn/article/cjfdtotal-ysxb200603002.htm
|
袁四化.冈底斯带中段北部早白垩世火山岩及其大地构造意义[D].中国地质科学院博士学位论文, 2009:1-110. http://cdmd.cnki.com.cn/article/cdmd-82501-2011012323.htm
|
高家昊, 曾令森, 高利娥, 等.西藏拉萨地体西北部革吉地区两期早白垩世岩浆作用——锆石U-Pb年龄、Hf同位素和地球化学特征[J].地质通报, 2016, 35(1):55-70. http://dzhtb.cgs.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20160106&journal_id=gbc
|
隋清霖.西藏拉萨地块盐湖地区早白垩世岩浆岩年代学、岩石成因及构造意义[D].中国地质大学(北京)硕士学位论文, 2014:1-65. http://cdmd.cnki.com.cn/article/cdmd-11415-1014239465.htm
|
谌微微.羌塘地块白垩纪火山岩和红层古地磁学和年代学新结果及其大地构造意义[D].中国地质大学(北京)博士学位论文, 2014:1-123.
|
张开均, 夏斌, 夏邦栋, 等.冈底斯弧弧后早白垩世裂谷作用的沉积学证据[J].沉积学报, 2003, 21(1):31-37. http://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200301005.htm
|
马国林, 岳雅慧.西藏拉萨地块北部白垩纪火山岩及其对冈底斯岛弧构造演化的制约[J].岩石矿物学杂志, 2010, 29(5):525-538. http://www.cnki.com.cn/Article/CJFDTOTAL-YSKW201005008.htm
|
陈明, 王剑, 谭富文, 等.西藏措勤盆地中侏罗世-早白垩世沉积充填特征[J].沉积与特提斯地质, 2005, 25(1):171-179. http://www.cnki.com.cn/article/cjfdtotal-ttsd2005z1030.htm
|
刘燊, 迟效国, 李才, 等.藏北新生代火山岩系列的地球化学及成因[J].长春科技大学学报, 2001, 31(3):232-235. http://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ200103005.htm
|
Zhai Q G, Huang X P. The fragment of Paleo-Tethys ophiolite from central Qiangtang, Tibet:geochemical evidence of metabasites in Guoganjianian[J]. Science in China(Series D), 2007, 50(9):1302-1309. doi: 10.1007/s11430-007-0051-7
Zhai Q G, Huang X P. The fragment of Paleo-Tethys ophiolite from central Qiangtang, Tibet:geochemical evidence of metabasites in Guoganjianian[J]. Science in China(Series D), 2007, 50(9):1302-1309. doi: 10.1007/s11430-007-0051-7
|
Zhai Q G, Wang J, Li C, et al. SHRIMP U-Pbdating and Hf isotopic analyses of Middle Ordovician meta-cumulate gabbro in central Qiangtang, northern Tibetan Plateau[J]. Science China Earh Science, 2010, 53:657-664. doi: 10.1007/s11430-010-0063-6
Zhai Q G, Wang J, Li C, et al. SHRIMP U-Pbdating and Hf isotopic analyses of Middle Ordovician meta-cumulate gabbro in central Qiangtang, northern Tibetan Plateau[J]. Science China Earh Science, 2010, 53:657-664. doi: 10.1007/s11430-010-0063-6
|
Pearce J A, Mei H. Volcanic rocks of the 1985 Tibet Geotraverse Lhasa to Golmud[J]. Royal Society of London Philosophical Transactions, Series A, 1988, 327:169-201. doi: 10.1098/rsta.1988.0125
Pearce J A, Mei H. Volcanic rocks of the 1985 Tibet Geotraverse Lhasa to Golmud[J]. Royal Society of London Philosophical Transactions, Series A, 1988, 327:169-201. doi: 10.1098/rsta.1988.0125
|
邓万明.青藏高原北部新生代板内火山岩[M].北京:地质出版社, 1998:1-180.
|
宋全友, 陈清华.青藏措勤盆地下白垩统则弄群火山岩岩石地球化学特征[J].石油大学学报, 1999, 23(5):17-19. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDX199905004.htm
|
刘伟, 李奋其, 袁四化, 等.西藏措勤地区则弄群火山岩源区——地球化学及Sr-Nd同位素制约[J].岩石矿物学杂志, 2010, 29(4) 367-376. http://www.cnki.com.cn/article/cjfdtotal-yskw201004002.htm
|
朱弟成, 莫宣学, 赵志丹, 等.西藏冈底斯带措勤地区则弄群火山岩锆石U-Pb年代学格架及构造意义[J].岩石学报, 2008, 24(3):401-412. http://industry.wanfangdata.com.cn/yj/Detail/Periodical?id=Periodical_ysxb98200803001
|
曲永贵, 刘贵忠, 郑春子, 等.西藏北部班戈地层分区下白垩统郎山组、康曲组和余穷组地层层序研究[J].地层学杂志, 2003, 27(3):220-226. http://www.cnki.com.cn/Article/CJFDTOTAL-DCXZ200303011.htm
|
彭少南.西藏革吉白垩系郎山组白云岩成因及储集性研究[D].中国地质大学(北京)硕士学位论文, 2010:1-71. http://cdmd.cnki.com.cn/article/cdmd-11415-2010085415.htm
|
王冠民.西藏措勤盆地郎山组沉积特征及其石油地质条件[J].地球学报, 2001, 22(1):39-42. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXB200101007.htm
|
王璞珺, Mattern F, Scheider W, 等.西藏班公湖-怒江缝合带白垩系沉积特征及其构造意义[J].世界地质, 2003, 22(2):105-110. http://www.wenkuxiazai.com/doc/f696c7b18762caaedd33d453-2.html
|
杜德道.西藏班公湖-怒江缝合带(中段和西段)的花岗岩地球化学特征及其构造环境[D].中国地质大学(北京)硕士学位论文, 2012:1-56.
|
李华亮.班公湖-怒江缝合带西段洋陆转换的标志及时间[D].中国地质大学(武汉)博士学位论文, 2014:1-93. http://cdmd.cnki.com.cn/article/cdmd-10491-1014340869.htm
|
许荣科, 茨邛, 庞振甲, 等. 中华人民共和国1∶25万区域地质调查报告(狮泉河幅). 2004. http://www.oalib.com/references/19254116
|