1.
The Closure Time of the Paleo-Asian Ocean and the Paleo-Tethys Ocean:Implication for the Tectonic Cause of the End-Permian Mass Extinction
古亚洲洋和古特提斯洋的闭合时代——论二叠纪末生物灭绝事件的构造起因
2.
Paleomagnetic Constraints on the Closure Time of Paleo-Tethys:Implications for the Tectonic Setting of Formation of Triassic Songpan-Ganzi Flysch Complex
古特提斯洋的闭合时代的古地磁分析:松潘复理石杂岩形成的构造背景
3.
THREE MESOZOIC SEA BASINS IN EASTERN AND SOUTHERN SOUTH CHINA SEA AND THEIR RELATION TO TETHYS AND PALEO-PACIFIC DOMAINS
南海中生代三期海盆及其与特提斯和古太平洋的关系
4.
(3) Post Caledonides platform also did not exist, there was an ocean basin and could be a part of the Paleo Tethys;
（3）华南不存在加里东后地台，而存在晚古生代洋盆，它可能是东特提斯洋的一部分；
5.
THE DISCOVERY AND TECTONIC SIGNIFICANCE OF A SMALL BRANCH OCEAN BASIN IN MONGGUBAO-PUSHOUYUAN,TETHYAN OCEAN OF NORTHERN KANGXIWA,WEST KUNLUN MOUNTAIN
西昆仑康西瓦北侧蒙古包—普守原特提斯洋一分支小洋盆的发现及构造意义
6.
PALEO-TETHYAN OPHIOLITES AND "THE NORTHERN BOUNDARY OF THE GONDWANALAND" IN THE QINGHAI-XIZANG TIBET PLATEAU
青藏古特提斯蛇绿岩与“冈瓦纳古陆北界”
7.
EDSA (Asia) Pacific Atlantis-The Representative of Holiday Facilities
大西洋(亚特兰提斯)——主体度假设施的代表作
8.
(3)MiddlePermian-Neogene extension-compression cycle of Neo-Tethys.
中二叠世---新近纪新特提斯洋构造域旋回。
9.
Discussing the Trace of Tythys in the Area from Northern Slope to the Boundary of Continent and Ocean of South China Sea;
南海北部陆坡—洋陆边界特提斯痕迹探讨
10.
Geological Characteristics of Lithofacies Paleogeography and Hydrocarbon Accumulation in Asian Tethyan Tectonic Domain
亚洲特提斯域岩相古地理与油气聚集地质特征
11.
PERMIAN-TRIASSIC PALEOCLIMATE OF EASTERN TETHYS AND ITS PALEOGEOGRAPHIC IMPLICATION
东特提斯地区二叠—三叠纪古气候特征及其古地理意义
12.
ACTIVE CONTINENTAL MARGIN AND REGIONALMETALLOGENESIS OF THE PALAEO-TETHYSIN THE EAST KUNLUN MOUNTAINS
古特提斯东昆仑活动陆缘及其区域成矿
13.
Triassic magmatism in the southern Lancangjiang zone,southwestern China and its constraints on the tectonic evolution of Paleo-Tethys
滇西古特提斯俯冲-碰撞过程的岩浆作用记录
14.
Since the beginning of the upper Triassic epoch, the Indian plate upthrusted to the north over the Tethys oceanic crust and led to the closure of the Tethys in Eocene epoch.
晚三迭世开始,印度板块在特提斯洋壳上向北仰冲,并导致特提斯在始新世的关闭。
15.
Is There a Neo-Tethys Subduction Record Earlier than arc volcanic rocks in the Sangri Group?
存在比桑日群弧火山岩更早的新特提斯洋俯冲记录么?
16.
Studying on the Carboniferous Sequence Stratigraphy of the Seamount Carbonate Platform in Paleo-Tethys,Southwestern Yunnan,China?
滇西南古特提斯石炭纪海山碳酸盐台地的层序地层学研究
17.
Volcanic Rocks in the Central Belt of Tethyan Himalayas Since the Late Paleozoic and Their Implications;
特提斯喜马拉雅带中段晚古生代以来的火山岩及其意义
18.
Geochemistry of the Permian basalt and its relationship with east Palaeo-Tethys evolution in Xiangyun area,Yunnan Province
滇西二叠系玄武岩及其与东古特提斯演化的关系