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| 1 | The Yanshanian Orogeny and Two Kinds of Yanshanides in Eastern-Central China显示文摘The Tan-Lu Fault was once a transform fault in the Paleotethys, west of which was the Qinling-Dabie Ocean separating the Yangtze Craton from the North China Craton, and east of which was the Su-Lu Ocean separating the Su-Wan Block from the Jiao-Liao Craton. The Qinling-Dabie Ocean closed in the Indosinian orogeny, which created the China-Southeast Asia Subcontinent, with the Tan-Lu Fault becoming a marginal shear zone along the newly-formed amalgamated subcontinent. The Su-Lu Ocean subducted partly in the Indosinian orogeny, but not closed. In the Jurassic and Early Cretaceous, the Su-Wan Block drifted northwards with subduction of the Su-Lu Ocean and moved westwards to converge the subcontinent by sinistral shearing of the ENE-striking fractures. The Su-Lu Ocean finally closed and the Su-Wan Block collided with the Jiao-Liao Craton in the Early Cretaceous, which constituted a part of the magnificent interplate Yanshanides. The interplate orogeny rejuvenated the fossil sutures and deep fractures, as well as the Indosinian orogen, and the intraplate (intracontinental) Yanshanian orogeny occurred in the subcontinent. The East Asia Yanshanides, consisting of the interplate orogens in the outer side and the intraplate orogens in the inner side, collapsed quickly in the latest Early Cretaceous and Late Cretaceous. The eastern China area entered a tensile period from the Eogene, and the tectonic differentiation between the central and eastern China areas since the Jurassic was further strengthened. | WU Genyao | 2005 | Acta Geologica Sinica(English Edition)2005，79，4： | 18 |
| 2 | Rejuvenation of Fossil Sutures and Related Mesozoic Intracontinental Orogenies in South China显示文摘The Huanan (South China) subcontinent was created by amalgamation of the Yangtze, Xianggan, Ca-thaysia and Zhemin microcontinents by the Guangxi orogeny in the Early Palaeozoic. The closure of the Tethyan Ocean and subsequent collision event outside the amalgamated continent reactivated fossil sutures and resulted in in-tracontinental (ensialic) orogenies in the Mesozoic. Based on evidence from deformation, molasse and granitoids, the Sichuan-Guizhou-Hunan-southern Hubei and Hunan-Jiangxi-Fujian Yanshanian fold-thrust systems and the Lower Yangtze-northwestern Fujian Indosinian fold-thrust system are thought to be intracontinental orogens. Their main features are as follows: intracontinental orogenies occurred areally, thrusting propagated towards the interior of the continental, they extend parallelly to the strikes of the fossil sutures, and the details of the temporal-spatial evolution of the orogens depend on subduction-collision events. | WU Genyao | 2000 | Acta Geologica Sinica(English Edition)2000，74，2： | 15 |
| 3 | Palinspastic reconstruction and geological evolution of Jurassic basins in Mongolia and neighboring China显示文摘The important event in Jurassic tectonics in Mongolia was the subduction and closure of the Mongolia-Okhotsk ocean;correspondingly,basin evolution can be divided into two main stages,related to the orogeny and collapse of the orogenic belt,respectively.The developing of Early-Middle Jurassic basins to the north of the ocean resulted from back-arc extension.The fossil sutures,from the China-SE Asia sub-continent to the south of the ocean,were rejuvenated by subduction-related orogeny;in addition,the Yanshanian intra-continental movement occurred.Three Early-Middle Jurassic molasse basins were developed by movement in Inner Mongolia,all of which stretched westwards (or northwards) into Mongolia;therefore,the molasse basins in eastern and southern Mongolia had the same geometric and kinematic features as the basins in the Inner Mongolia.Owing to the collapse of the MongoliaOkhotsk orogenic belt,a group of rift basins developed during the Late Jurassic.In eastern Mongolia,the NE orientated extensional basins were controlled by the neogenic NE-structure.The contemporary basins in southern Mongolia and the neighboring areas in China were constrained by remobilization (inherited activation) of the latitudinal or ENE-directional basement structures.Three stages can be recognized in the evolution of the Early-Middle Jurassic basins after reversal;the basins also experienced four episodes of reformation. | Wu Genyao | 2013 | Journal of Palaeogeography2013，2，3： | 12 |
| 4 | Discovery of ophiolite in southeast Yunnan,China显示文摘The Babu ophiolite in Malipo County, SE Yunnan, consists of three units: ultramafic, mafic and basaltic rocks. Studies of geological mapping, petrology and geochemistry reveal that the gabbro is similar to that in the Troodos ophiolite, and the diabase and basalt belong to a normal MORB-type,analogous to the Shuanggou ophiolite in west Yunnan. The ophiolite studied as a thrust tectonic slab,was overthrust northwards onto the Late Paleozoic-Triassic deep marine deposits of continental margin.It is inferred to be relics of Paleotethyan ocean; namely, a branch of Paleotethys occurs in South China, where the tectonic nature and evolutional history of the area should be reconsidered. | Dalai Zhong Genyao Wu Jianqing Ji Qi Zhang Lin Ding | 1999 | Chinese Science Bulletin1999，44，1： | 8 |
| 5 | Indosinian Foreland Fold-and-Thrust Belt Bordering Yunnan and Guangxi, China显示文摘Recent discoveries of ophiolites indicate that there must be aPalaeotethyan geosuture zone bordering China and Vietnam, which separates the Vietbac block from the South China subcontinent. The Indosinian foreland fold-and thrust belt bordering Yunnan and Guangxi provided further evidence for the palaeotethysides. The oceanic crust was subducted southwestwards while the magmatic arc migrated northeastwards, and the continent-arc collision occurred in the Late Triassic with the thrusting being extended towards the north or northeast. The features of thrust-nappe structure are discussed, which proved the continental margin of the Palaeotethyan ocean there to be a complicated one. A face-to face collision occurred first along the NW-striking segment and then along the ENE-striking segment accompanied by transpression or oblique thrusting occurring along the NW-striking one. | WU Genyao Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029 | 2001 | Acta Geologica Sinica(English Edition)2001，75，4： | 3 |
| 6 | Pet- rologic and geochemical constraints on the petrogenesis of Permian-Triassic Emeishan flood basalts in southwestern China 显示文摘 | Xu Yigang Chung Sun-lin Jahn Bor-ming Wu Genyao | 2001 | Lithos2001，58，34： | 1 |
| 7 | Yanshanian orogenics in South China: a relation to Neotethyan evolution显示文摘 | Wu Genyao Yano T Inomata M | 1998 | Seientia Geologica Siniea1998，7，1： | 1 |
| 8 | Babu-Phu Ngu ophiolite: A geological record of Paleotethyan ocean bordering China and Vietnam 显示文摘 | Wu Genyao Zhong Dalai Zhang Qi | 1999 | Gondwana Research1999，2，4： | 1 |
| 9 | Laochang volcanics:a record of Azores-type oceanic islands in Paleotethys,southwestern Yunnan显示文摘 | Wu Genyao | 1994 | Scientia Geologica Sinica1994，3，1： | 1 |
| 10 | Tectono-sedimentary development of backarc continental basin in Yunnan, southern China显示文摘 | Yano T Wu Genyao Tan Mingqing | 1994 | Jour SE Asian Earth Science1994，9，12： | 1 |
| 11 | Petrological and geochemical constraints on the petrogenesis of the Permo-Triassic Emeishan flood basalts in southwestern China 显示文摘 | Chung S L Jahn B M Genyao Wu | 2001 | Lithos2001，58，： | 1 |
| 12 | Yanshanian orogenics in South China: a relation to Neotethyan evolution显示文摘 | Wu Genyao Yano T Inomata M | 1998 | Scientia Geologica Sinica1998，7，1： | 1 |
| 13 | Tectono-sedimentary development of Jinggu pull-apart basin in southwestern Yunnan, China显示文摘 | Liu Shanyin Wu Genyao Zhong Dalai | 1996 | Scientia Geologica Sinica1996，5，1： | 1 |
| 14 | Late Paleozoic tectonic framework and Paleotethyan evolution in western Yunnan,China显示文摘 | Wu Genyao | 1993 | Scientia Geologica Sinica1993，2，2： | 1 |
| 15 | Petrologic and geochemical constraints on the petrogenesis of Permian–Triassic Emeishan flood basalts in southwestern China显示文摘 | Yigang Xu Sun-Lin Chung Bor-ming Jahn Genyao Wu | 2001 | LITHOS2001，，3： | 1 |
| 16 | Laochang volcanics:a record of Azores-type oceanic islands in Paleotethys,southwestern Yunnan显示文摘 | Wu Genyao | 1994 | Scientia Geologica Sinica1994，3，1： | 1 |
| 17 | Petrologic and geochemical constraints on the petrogenesis of Permian–Triassic Emeishan flood basalts in southwestern China显示文摘 | Yigang Xu Sun-Lin Chung Bor-ming Jahn Genyao Wu | 2001 | LITHOS2001，，3： | 1 |
| 18 | Late Paleozoic tectonic framework and Paleotethyan evolution in western Yunnan,China显示文摘 | Wu Genyao | 1993 | Scientia Geologica Sinica1993，2，2： | 1 |
| 19 | Yanshanian orogenics in South China:a relation to Neotethyan evolution显示文摘 | Wu Genyao Yano T Inomata M | 1998 | Scientia Geologiea Sinica1998，7，1： | 1 |
| 20 | Yanshanian orogenics in South China:a relation to Neotethyan evolution显示文摘 | Wu Genyao Yano T Inomata M | 1998 | Scientia Geologica Sinica1998，7，1： | 1 |
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