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| 1 | Deformation Stages and Ar-Ar Age Data of the Wan-Zhe-Gan Tectonic Zone,Southeast China,and Their Tectonic Significance显示文摘在东南中国通过安徽,浙江,和江西省的边阶区域的主要构造地区通常被叫作 Wan-Zhe-Gan 差错地区。地质上,这个地区由各种各样的年龄和取向的几条地区性的差错带组成。我们基于地调查把差错分成了四个年龄组。Neoproterozoic 差错向东北正在罢工。他们从东北江西省开始并且延长对在安徽省的 Fuchuan 向东北,东北 Jiangxi-Fuchuan ophiolite 带的一样的地点。可能作为一条边界在 Neoproterozoic 期间扮演的差错与 m 指责一个盘子或块缝术的地区 ???? | YU Xinqi WANG De'en JIANG Dazhi JIANG Laili ZHOU Xiang LI Chunlin | 2011 | Acta Geologica Sinica(English Edition)2011，85，6： | 10 |
| 2 | Tectono-sedimentary Evolution of Piggy-Back Basin:Example from Kuqa Fold and Thrust Belt,Northern Tarim Basin,Northwest China显示文摘The Baicheng(拜城) piggy-back basin was part of the intracontinental foreland basin system of southern Tianshan(天山) Mountains.It was formed on a thrust-and-fold belt induced by Mio-Pliocene collision between southern Tianshan Mountains and Tarim craton that controlled the thick synorogenic basin fills.Sedimentological analysis and a restored cross-section based on seismic data and field studies revealed three tectono-depositional sequences of synorogenic basin fills.(1) The Lower Miocene sequence(Jidike(吉迪克) Formation) was formed under alluvial-braided river-lacustrine environments,in response to geodynamic changes of the Kuqa(库车) fold and thrust belt from the embryonic foreland to a foredeep in the course of orogenic loading period.(2) The Upper Miocene sequence(Kangcun(康村) Formation) was developed in fluvial-delta and lacustrine environments,within a foredeep due to orogenic thrust.(3) The Pliocene sequence(Kuqa Formation) was formed in the Baicheng piggy-back basin that became a wedge-top depozone,thrusting in the Qiulitagh(秋里塔格) thrust belt that propagated progressively southward to the Yaken(牙肯) thrust belt. | 杨明慧 金之钧 吕修祥 孙冬胜 曾鹏 | 2010 | Journal of Earth Science2010，21，4： | 0 |
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