Citation: | YANG Yunjun, HAN Xu, BIAN Xiaowei, ZHANG Manshe, ZHANG Mingyun. An analysis of sedimentary environment and prototype basin of Lueyang Group in the Mian-Lue-Ning triangle area Shaanxi Province[J]. Geological Bulletin of China, 2020, 39(10): 1549-1560. |
Lueyang Group sedimentary rock of the Late Paleozoic is located in the Mian-Lue-Ning triangle area, Shaanxi Province. It is mainly distributed in the east of Motianling block and Mian-Lue suture of South Qinling Mountain. According to field survey, there are differences in sedimentary environment and Prototype basin. Lueyang Group. is characterized by wide distribution, complex rock assemblage and diverse sedimentary environment. The rhythm-cyclic sedimentary sequence composed of coarse to fine clastic rocks developed in Tapo Formation can be divided into three sections. The lower section includes the coarse clastic rocks from alluvial fan of different source areas, and the ancient water direction is from south to north; the middle-upper section is characterized by the sedimentary deposits of the middle-high grained clastic rocks, which represent the delta environment. Lueyang Formation consists of carbonate platform facies and slope facies. The sedimentary action and material records represented by the Tapo Group marked the deposition events of late Paleozoic rifting and confined stabilization basin background on the east margin of the Motianling block and Mian-Lue suture. The research has great significance in the study of tectonic evolution in Mian-Lue-Ning triangle area.
[1] | 张国伟, 张本仁, 袁学诚, 等.秦岭造山带与大陆动力学[M].北京:科学出版社, 2001:1-855. |
[2] | 杨运军, 杜少喜, 张小明, 等.陕西勉略宁三角区碧口群火山岩系特征及其地质填图方法探讨[J].西北地质, 2017, 50(3):105-112. |
[3] | 杨运军, 于恒彬, 游军, 等.陕西勉略宁三角区弧后裂解型火山岩特征及其构造意义[J].矿产勘查, 2018, 9(9):1768-1778. |
[4] | 孟庆任, 张国伟, 于在平, 等.秦岭南缘晚古生代裂谷——有限洋盆沉积作用及构造演化[J].中国科学(D辑), 1996, (S1):28-33. |
[5] | 孟庆任.秦岭的由来[J].中国科学:地球科学, 2017, 47(4):412-420. |
[6] | 杜远生, 盛吉虎, 冯庆来, 等.南秦岭勉略地区"三河口群"的解体及地质意义[J].地层学杂志, 1998, 22(3):170-175. |
[7] | 杜远生.西秦岭造山带泥盆纪沉积地质学和动力沉积学研究:西秦岭南带泥盆纪裂陷槽盆地、摩天岭地体沉积特征和盆地格局[J].岩相古地理, 1995, 3(6):48-61. |
[8] | 杜远生, 盛吉虎, 韩欣, 等.南秦岭勉(县)略(阳)构造混杂岩带的泥盆纪-石炭纪古海洋演化[J].古地理学报, 1999, (4):54-60. |
[9] | 杨志华, 王训练, 周洪瑞, 等.南秦岭略阳地区略阳组牙形刺新材料及其时代意义[J].微体古生物学报, 2019, 36(1):87-96. |
[10] | Yan Q R, Wang Z Q, Han son A D, et al.SHRIMP age and geochemistry of Bikou volcanic terrane:implication for Neoproterozoic tect onics on the north margin of the Yangtze craton[J].Acta Geoscientica Sinica, 2003, 77(4):479-490. |
[11] | Dong Y P, Zhang G W, Neubarer F, et al.Tectonic evolution of the Qinling Orogen, China:Review and synthesis[J].J.Asian Earth Sci.2011, 41:213-237. doi: 10.1016/j.jseaes.2011.03.002 |
[12] | 裴先治.勉略-阿尼玛卿构造带的形成演化与动力学特征[D].西北大学博士学位论文, 2001. |
[13] | 杨志华, 李勇, 邓亚婷.勉略带是古生代的板块缝合带吗?[J].湖北地矿, 2001, 15(2):11-17. |
[14] | 张拴厚, 韩芳林, 王根宝, 等.中国区域地质志·陕西志[M].北京:地质出版社, 2017. |
[15] | 杜定汉.陕西秦巴地区泥盆系研究[M].西安:西安交通大学出版社, 1986:1-187. |
[16] | 马润华, 伊鹍英, 王振东, 等.陕西省岩石地层[M].武汉:中国地质大学出版社, 1998. |
[17] | Follo M F.Conglomerates as clues to the sedimentary and tectonic evolution of a suspect terrane:Wallowa Mountains, Oregon[J].Geological Society of America Bulletin, 1992, 104:1561-1576. doi: 10.1130/0016-7606(1992)104<1561:CACTTS>2.3.CO;2 |
[18] | Dickinson W R, Beard L S, Brakenridge G R, et al.Provenance of North Ametican Phanerozoic sandstones in relation to tectonic settings[J].Geologacal Society of America Bulletin, 1983, 93:222-235. |
[19] | Ingersoll R V, Busby C J.Tectonics of sedimentary basins[M].Black-well Science, 1995:1-51. |
[20] | 马润华, 伊眼英, 王振东, 等.陕西省岩石地层[M].武汉:中国地质大学出版社, 1998. |
[21] | 金同安.对略阳灰岩时代的一点认识[J].西北地质, 1983, 4:51-66. |
[22] | 张克信, 何卫红, 徐亚东, 等.沉积大地构造相划分与鉴别[J].地球科学-中国地质大学学报, 2014, 39(8):915-928. |
[23] | 张国伟, 程顺有, 郭安林, 等.秦岭-大别中央造山系南缘勉略古缝合带的再认识——兼论中国大陆主体的拼合[J].地质通报, 2004, 23(9/10):846-853. |
[24] | 赖绍聪, 张国伟, 杨永成, 等.南秦岭勉县-略阳结合带蛇绿岩与弧火山岩地球化学及其大地构造意义[J].地球化学, 1998, 27(3):283-292. |
[25] | 徐学义, 夏祖春, 夏林圻.碧口群火山旋回及其地质构造意义[J].地质通报, 2002, (Z2):478-485. |
[26] | 李亚林, 李三忠, 张国伟.秦岭勉略缝合带组成与古洋盆演化[J].中国地质, 2002., 29(2):129-134. |
[27] | 夏林圻, 夏祖春, 徐学义, 等.碧口群火山岩岩石成因研究[J].地学前缘, 2007, 14(3):84-101. |
[28] | 闫全人, Hanson A D, 王宗起, 等.扬子板块北缘碧口群火山岩的地球化学特征及其构造意义[J].岩石矿物学杂志, 2004, 23(1):1-11. |
[29] | Druschke P A, Hanson A D, Yan Q R, et al.Stratigraphic and U-Pb SHRIMP detrital zircon evidence for a Neoproterozoic continental arc, central China:Rodinia implications[J].The Journal of Geology, 2006, 114:627-636. doi: 10.1086/506162 |
[30] | Xiao L, Zhang H F, Ni P Z, et al.LA-ICP-MS U-Pb zircon geochronology of early Neoproterozoic mafic-intermedidiat intrusions from margin of the Yangtze Block, South China:Implication fou tectonic evolution[J].Precambrian Reseath, 2007, 154:221-235. doi: 10.1016/j.precamres.2006.12.013 |
[31] | 任纪舜, 朱俊宾, 李崇, 等.秦岭造山带是印支碰撞造山带吗?[J].地球科学.2019, 44(5):1476-1486. |
[32] | 张宗清, 张国伟, 付国民, 等.秦岭变质地层年龄及其构造意义[J].中国科学(D辑), 1996, (3):216-222. |
[33] | 匡耀求, 张本仁, 欧阳建平.扬子克拉通北西缘碧口群的解体与地层划分[J].地球科学——中国地质大学学报, 1999, 24(3):251-255. |
[34] | 王涛, 王宗起, 闫臻, 等.南秦岭大堡组奥陶纪洋岛玄武岩的识别及其构造意义:来自地球化学和年代学证据[J].岩石学报, 2009, 25(12):3241-3250. |
[35] | 李瑞保, 裴先治, 丁仨平, 等.西秦岭南缘勉略带琵琶寺基性火山岩LA-ICP-MS锆石U-Pb年龄及其构造意义[J].地质学报, 2009, 83(11):1612-1623. |
[36] | 李佐臣.扬子板块西北缘后龙门山造山带(北段)物质组成、构造特征及其形成演化[D].长安大学博士学位论文, 2009. |
[37] | 徐通, 裴先治, 李瑞保, 等.勉略构造带横现河地区张岩沟双峰式火山岩的地球化学特征、LA-ICP-MS锆石U-Pb年龄及其构造意义[J].中国地质, 2013.40(6):1777-1792. |
[38] | 秦克令, 金浩甲, 赵东宏.碧口群古岛弧带构造演化与成矿[J].河南地质, 1994, 12(4):304-317. |
[39] | 汪新伟, 沃玉进, 张荣强.扬子克拉通南华纪-早古生代的构造-沉积旋回[J].现代地质, 2008, 22(4):525-533. |
[40] | 杨明桂, 祝平俊, 熊清华, 等.新元古代-早古生代华南裂谷系的格局及其演化[J].地质学报, 2012, 86(9):1367-1375. |
[41] | 刘宝珺, 许效松, 徐强.扬子东南大陆边缘晚元古代-早古生代层序地层和盆地动力演化[J].岩相古地理, 1995, 5(3):1-16. |
[42] | 冯益民, 曹宣铎, 张二朋.勉县-略阳带大地构造属性之探讨[J].地质论评, 2004, 50(3):295-303. |
① | 杨运军, 张小明, 胡义, 等.陕西省勉略宁地区基础地质调查成果报告.2018. |
② | 王训练, 周洪瑞, 沈阳, 等.略阳群地层特征及构造意义专题研究报告.2018. |
③ | 吴闻人, 王永和, 王根宝, 等.郭镇-何家岩地区1: 5万区调联测报告.地矿部陕西地质矿产勘查开发局, 1996. |
④ | 何建社, 蔺新望, 王金安, 等.1: 25万略阳幅区域地质调查报告.2007. |
⑤ | 1: 20万略阳幅区域地质调查报告.陕西省地矿局区域地质调查队, 1991. |
Tectonic location (a) and regional geological map (b) of Mian-Lue-Ning area
Geological section of the Tianba-Changba Devonian Tapo Formation, Lueyang County
Graded bedding (a), geopetal structure (b) and stamping die structure (c) of Tapo Formation
Statistics of Tapo Formation conglomerate
Discriminant diagrams of the tectonic background of Tapo sandstone Q-F-L, Lueyang
Geological section of the upper section of Lueyang Formation from Baiya ditch, Douba Township, Kangxian County
Geopetal structure of the Lueyang Formation (a), small and medium mudstone soft sedimentary deformation (b) and astroies (c)
Late Tournaisian conodontic microbody fossils, Zhujiadong
Stratigraphic correlation and sedimentary evolution diagram of Lueyang Group