Abstract：The Early Paleozoic Hongliugou- Lapeiquan ophiolite melange zone is an important tectonic boundary in northern Altyn area. It is a key area for studying the subduction boundaries, tectonic evolution and regional framework reconstruction because of complex compositions, rich structures and frequent magmatism. During the 1:50 000 regional geological survey in Annanba of northern Altyn area, the spatial extension, material composition, textures and structures of the Hongliugou- Lapeiquan ophiolite melange zone have been revealed according to tectonic- lithologic mapping. Based on comprehensive study of typical structural profile and deformation events, the tectonic evolution of Altyn area in Early Paleozoic is discussed, which provides a theoretical possibility for establishing a structural model for general melange.
查显锋,李荣社,辜平阳,计文化,陈锐明,张海迪. 北阿尔金红柳沟-拉配泉构造混杂岩带东段的结构、构造[J]. 中国地质调查, 2015, 2(8): 35-42.
ZHA Xian-feng, LI Rong-she, GU Ping-yang, JI Wen-hua, CHEN Rui-ming, Zhang Hai-di. Textures and Structures in the Eastern Hongliuguou-Lapeiquan Tectonic Melange Zone of Northern Altyn Area. , 2015, 2(8): 35-42.
[1] 李继亮.增生型造山带的基本特征[J].地质通报,2004,23(9/10):947-951. [2] 索书田.造山带的网结状构造样式[J].地质科技情报,1993,12(2):1-7. [3] 王克卓,李嵩龄,李文铅,等.东准噶尔蛇绿混杂岩带填图等级体制划分意见讨论[J].新疆地质,1999,17(4):337-343. [4] 张克信,殷鸿福,朱云海,等.造山带混杂岩区地质填图理论、方法与实践——以东昆仑造山带为例[M].武汉:中国地质大学出版社,2001:13-27. [5] 张克信,冯庆来,宋博文,等.造山带非史密斯地层[J].地学前缘,2014,21(2):36-47. [6] 李荣社,计文化,辜平阳,等.构造混杂岩带填图的几点建议[C]//第五届全国构造地质与地球动力学学术研讨会,论文摘要集(专题5).武汉:中国地质学会,2012:266-267. [7] 张建新,许志琴,徐惠芬,等.北祁连加里东期俯冲-增生楔结构及动力学[J].地质科学,1998,33(3):290-299. [8] 朱云海,潘元明,张克信,等.蛇绿岩就位机制研究[J].地质科技情报,2000,19(1):16-18. [9] 肖文交,周辉,Windley B F,等.西昆仑造山带复式增生楔的构造特征与演化[J].新疆地质,2003,21(1):31-36. [10] Xiao W J,Zhang L C,Qin K Z,et al.Paleozoic accretionary and collisional tectonics of the Eastern Tianshan (China):Implications for the continental growth of central Asia[J].American Journal of Science,2004,304(4):370-395. [11] Xiao W J,Windley B F,Allen M B,et al.Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage[J].Gondwana Research,2013,23(4):1316-1341. [12] Grando G, McClay K.Morphotectonics domains and structural styles in the Makran accretionary prism,offshore Iran[J].Sedimentary Geology,2007,196(1-4):157-179. [13] Braid J A,Murphy J B,Quesada C.Structural analysis of an accretionary prism in a continental collisional setting,the Late Paleozoic Pulo do Lobo Zone,Southern Iberia[J].Gondwana Research,2010,17(2/3):422-439. [14] Charvet J.Late Paleozoic-Mesozoic tectonic evolution of SW Japan:a review-Reappraisal of the accretionary orogeny and revalidation of the collisional model[J].Journal of Asian Earth Sciences,2013,72:88-101. [15] 刘良,车自成,王焰,等.阿尔金高压变质岩带的特征及其构造意义[J].岩石学报,1999,15(1):57-64. [16] 吴峻,兰朝利,李继亮,等.阿尔金红柳沟蛇绿混杂岩中MORB与OIB组合的地球化学证据[J].岩石矿物学杂志,2002,21(1):24-30. [17] 杨经绥,吴才来,史仁灯.阿尔金山米兰红柳沟的席状岩墙群:海底扩张的重要证据[J].地质通报,2002,21(2):69-74. [18] 车自成,刘良,罗金海.中国及其邻区区域大地构造学[M].北京:科学出版社,2002:207-369. [19] 郝杰,王二七,刘小汉,等.阿尔金山脉中金雁山早古生代碰撞造山带:弧岩浆岩的确定与岩体锆石U-Pb和蛇绿混杂岩40Ar/39Ar年代学研究的证据 [J].岩石学报,2006,22(11):2743-2752. [20] 修群业,于海峰,刘永顺,等.阿尔金北缘枕状玄武岩的地质特征及其锆石U-Pb年龄[J].地质学报,2007,81(6):787-794. [21] 张建新,孟繁聪,于胜尧,等.北阿尔金 HP/LT 蓝片岩和榴辉岩的Ar-Ar年代学及其区域构造意义[J].中国地质,2007,34(4):558-564. [22] 杨经绥,史仁灯,吴才来,等.北阿尔金地区米兰红柳沟蛇绿岩的岩石学特征和SHRIMP定年[J].岩石学报,2008,24(7):1567-1584. [23] 高晓峰,校培喜,过磊,等.北阿尔金地区早古生代有限洋盆开启时限:来自斜长花岗岩的证据[J].中国科学:地球科学,2012,42(3):359-368. [24] 刘良,车自成,王焰,等.阿尔金茫崖地区早古生代蛇绿岩的Sm-Nd 等时线年龄证据[J].科学通报,1998,43(8):880-883. [25] 张建新,张泽明,许志琴,等.阿尔金构造带西段榴辉岩的 Sm-Nd 及 U-Pb 年龄:阿尔金构造带中加里东期山根存在的证据[J].科学通报,1999,44(10):1109-1112. [26] Zhang J X,Zhang Z M,Xu Z Q,et al.Petrology and geochronology of eclogites from the western segment of the Altyn Tagh,northwestern China[J].Lithos,2001,56(2):187-206. [27] 边千韬,赵大升,叶正仁,等.初论昆祁秦缝合系[J].地球学报,2002,23(6):501-508. [28] 李荣社,计文化,陈守建,等.青藏高原及邻区古生代构造-岩相古地理图(1:3 000 000) [M].北京:地质出版社,2012:73-74. [29] 查显锋,辜平阳,计文化,等.欧龙布鲁克地块西段达肯大坂岩群物质组成及变形特征研究[J].地质科学,2013,48(4):1103-1114. [30] 陆松年,于海峰,李怀坤,等.“中央造山带”早古生代缝合带及构造分区概述[J].地质通报,2006,25(12) :1368-1380. [31] 吴珍汉,胡道功,宋彪,等.柴达木盆地北缘达肯大坂片麻岩锆石离子探针U-Pb同位素测年[J].地球学报,2007,28(1):1-6. [32] 吴才来,杨经绥,许志琴,等.柴达木盆地北缘古生代超高压带中花岗质岩浆作用[J].地质学报,2004,78(5):658-674. [33] 孟繁聪,张建新,杨经绥.柴北缘锡铁山早古生代HP/UHP变质作用后的构造热事件——花岗岩和片麻岩的同位素与岩石地球化学证据[J].岩石学报,2005,21(1):45-56. [34] 陈宣华,Gehrels G E,王小凤,等.阿尔金山北缘花岗岩的形成时代及其构造环境探讨[J].矿物岩石地球化学通报,2003,22(4):294-298. [35] Liu Y J,Ye H W,Ge X H,et al.Laser probe 40Ar/39Ar dating of mica on the deformed rocks from Altyn Fault and its tectonic implications,western China[J].Chinese Science Bulletin,2001,46(4):322-325. [36] 刘永江,葛肖虹,Genser J,等.阿尔金断裂带构造活动的40Ar/39Ar年龄证据[J].科学通报,2003,48(12):1335-1341. [37] 刘永江,Neubauer F,葛肖虹,等.阿尔金断裂带年代学和阿尔金山隆升[J].地质科学,2007,42(1):134-146,188. [38] 张岳桥,陈正乐,杨农.阿尔金断裂晚新生代左旋走滑位错的地质新证据[J].现代地质,2001,15(1):8-12. [39] 陈正乐,张岳桥,王小凤,等.新生代阿尔金山脉隆升历史的裂变径迹证据[J].地球学报,2001,22(5):413-418. [40] 陈宣华,尹安,Gehrels G E,等.青藏高原北缘中生代伸展构造40Ar/39Ar 测年和MDD模拟[J].地球学报,2002,23(4):305-310. [41] 葛肖虹,刘永江,任收麦.青藏高原隆升动力学与阿尔金断裂[J].中国地质,2002,29(4):346-350. [42] 刘永江,叶惠文,葛肖虹,等.阿尔金断裂变形岩激光微区40Ar/39Ar年龄及其构造意义[J].科学通报,2000,45(19):2101-2104. [43] 葛肖虹,刘永江,任收麦,等.对阿尔金断裂科学问题的再认识[J].地质科学,2001,36(3):319-325. [44] Liu Y J,Neubauer F,Genser J,et al.Geochronology of the initiation and displacement of the Altyn Strike-Slip Fault,western China[J].Journal of Asian Earth Sciences,2007,29(2-3):243-252. [45] 袁四化,刘永江,葛肖虹,等.青藏高原北缘的隆升时期——来自阿尔金山和柴达木盆地的证据[J].岩石矿物学杂志,2008,27(5):413-421.
2015, Vol. 2 
