|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Chinese Continental Blocks in Global Paleocontinental Reconstruction during Paleozoic and Mesozoic显示文摘对从中国大陆人和邻近的块的白垩纪 paleomagnetic 数据寒武纪用原则被收集获得可靠、高精确的 paleomagnetic 数据并且注意 paleobiogeography 和构造进化的协作的类似。中国大陆人块在建议全球 paleocontinents 的重建上被贮藏与几乎一样的规模。因此,包括中国大陆人块,全球大陆在赤道的南部的方面上沿着纬度变化在期间,这能清楚地被认出早古生代。在古生代的、中国大陆人,块仍然在 Laurentia ,西伯利亚和 Gondwana 盘子之中位于,跟随向北的西伯利亚板的快移动,在在 Laurentia 和 Gondwana 盘子的西方的部分的一个纵贯的方向的合并,和 Iapetus 和 Rheic 海洋是 subducted ,最后形成一致 Pangea 在晚古生代。东方 Gondwana 的澳大利亚、印度的盘子向南逐渐地移动了并且分散,继续扩大 Paleo-Tethys 海洋。中国大陆人和邻近的块仍然位于 Paleo-Tethys 海洋,保存了分散的地位,逐渐地向北移动,沿着 northsouth 取向变化直到的出现特征二叠。另外,一系列本地碰撞发生了在期间三叠纪,并且因而,大多数中国大陆人块被混合进 Pangea,除了 Gangdise 和喜玛拉雅的块。有在侏罗记的东方亚洲大陆的逆时针方向的旋转,向北,在在白垩纪期间改变度的中国大陆的移植,而是喜玛拉雅、印度的盘子没在这个时期期间碰撞进中国大陆。 | WAN Tianfeng ZHU Hong | 2011 | Acta Geologica Sinica(English Edition)2011，85，3： | 17 |
| 2 | The genesis of tectono-magmatism in eastern China显示文摘The tectono-magmatism in eastern China is a hotspot for the researches, and many hypotheses of that were discussed. There is a middle crust with solid, low velocity and high conductivity in eastern China, which is impossible to form'convection magmatic layer'. The subduction and compression of oceanic plate induced to the lateral pressure for the eastern China lithosphere in the condition of increasing pressure and decreasing temperature, it is also impossible to form an extensively melting magma layer. In South China, the granitic zone migrates from west to east, their evolution cannot be explained by plate subduction. The original magmatic reservoirs are controlled by main faults and spheres, which occurred the tectonic detachment and formed in the process of decreasing pressure and increasing temperature. The magma only originates in very small part of lithosphere. The tectono-magmatism and tectonic detachment of eastern China lithosphere during the Jurassic and the Cretaceous are concentrate mainly near the intersections between the regional faults and middle crust or the Moho discontinuity, and then magma intrudes or erupts along faults. The tectono-magmatism of Cenozoic originates near the intersections between the regional high-angle normal faults and the bottom of lithosphere. Obviously, the different penetration depth of faults induces a different kind of magmatism. | WAN TianFeng ZHAO QingLe | 2012 | Science China Earth Sciences2012，55，3： | 14 |
| 3 | Paleozoic Tectono-Metallogeny in the Tianshan-Altay Region,Central Asia显示文摘The research on Paleozoic tectonics and endogenic metallogeny in the Tianshan-Altay region of Central Asia is an important and significant project. The Altay region, as a collision zone of the Early Paleozoic(500–397 Ma), and the Tianshan region, as a collision zone of the early period in the Late Paleozoic(Late Devonian-Early Carboniferous, 385–323 Ma), are all the result of nearly N-S trending shortening and collision(according to recent magnetic orientation). In the Late Devonian-Early Carboniferous period(385–323 Ma), regional NW trending faults displayed features of dextral strike-slip motion in the Altay and Junggar regions. In the Tianshan region, nearly EW-trending regional faults are motions of the thrusts. However, in the Late Carboniferous-Early Permian period(323–260 Ma), influenced by the long-distance effect induced from the Ural collision zone, those areas suffered weaker eastward compression, the existing NW trending faults converted into sinistral strike-slip in the Altay and Junggar regions, and the existing nearly E-W trending faults transferred into dextral strike-slip faults in the Tianshan region. The Rocks of those regions in the Late Carboniferous-Early Permian period(323–260 Ma) were moderately ruptured to a certain tension-shear, and thus formed a number of world famous giant endogenic metal ore deposits in the Tianshan-Altay region. As to the Central Asian continent, the most powerful collision period may not coincide with the most favorable endogenic metallogenic period. It should be treated to 'the orogenic metallogeny hypothesis' with caution in that region. | WAN Tianfeng ZHAO Qingle WANG Qianqian | 2015 | Acta Geologica Sinica(English Edition)2015，89，4： | 6 |
| 4 | Mesozoic-Cenozoic Tectonics of the Yellow Sea and Oil-Gas Exploration显示文摘The purpose of the present study was to study the tectonics of the Yellow Sea. Although oil- gas exploration has been undertaken for more than 30 years in the southern Yellow Sea, the exploration progress has achieved little. There are three tectonic periods with near N–S trending shortening and compression (260–200 Ma, 135–52 Ma and 23–0.78 Ma) and three tectonic periods with near E–W trending shortening and compression (200–135 Ma, 52–23 Ma and 0.78 Ma) at the Yellow Sea and adjacent areas during the Mesozoic and Cenozoic. The Indosinian tectonic period is the collision period between the Sino-Korean and Yangtze Plates, which formed the basic tectonic framework for the Yellow Sea area. There were strong intraplate deformations during the Yanshanian (200–135 Ma) and Sichuanian (135–52 Ma) periods with different tectonic models, which are also the main formation periods for endogenic metallic mineral deposits around the Yellow Sea. The three tectonic periods during the Cenozoic affect important influences for forming oil-gas reservoirs. The Eocene–Oligocene (52–23 Ma) is the main forming period for oil-gas sources. The Miocene–Early Pleistocene (23–0.78 Ma) was a period of favorable passage for oil-gas migration along NNE trending faults. Since the Middle Pleistocene (0.78 Ma) the NNE trending faults are closed and make good conditions for the reservation of oil-gas. The authors suggest that we pay more attention to the oil-gas exploration at the intersections between the NNE trending existing faults and Paleogene– Neogene systems in the southern Yellow Sea area. | WAN Tianfeng HAO Tianyao | 2010 | Acta Geologica Sinica(English Edition)2010，84，1： | 4 |
| 5 | Cretaceous-Early Eocene Tectonic Stress Field in China显示文摘The Cretaceous-early Eocene tectonic stress field in China was reconstructed using the data of 369 largeand medium-scale flexural folds and 157 joint sets. It was found that the maximum compressive principal stress axis in eastern China dips 32° NE (nearly horizontal), and strikes SW 212°, whereas that in western China dips 15° NE (also nearly horizontal) and trends SW 195°. The estimation of the dip angles of fold limbs and the palaeotectonic stress values indicates that there was a tendency of gradual weakening of tectonism from southwestern to northeastern China in the Cretaceous-early Eocene. At the depth of 2-3 km, the differential stress value changes from 183 MPa in Tibet to 100 MPa in North and East China.The authors consider that the tectonic stress of this period was related to the north-northeastward movement and push of the Indian-Australian plate. | Wan Tianfeng and Zhu Hong China University of Geosciences, Beijing, China | 1989 | Acta Geologica Sinica(English Edition)1989，63，3： | 2 |
| 6 | Tectonic characteristics of the central segment of the Tancheng-Lujiang fault zone, Shandon Peninsula, eastern China显示文摘 | Lin Aiming Miyata T Wan Tianfeng | 1998 | Tectonophysics1998，293，： | 1 |
| 7 | Clarification of the geophysical definition of a gravity field显示文摘 | Hualin Zeng Tianfeng Wan | 2004 | Geophysics2004，69，： | 1 |
| 8 | On the extraterrestrial impact and plate tectonic dynamics: A possible interpretation 显示文摘 | Wan Tianfeng Yin Yanhong Zhang Changhou | 1997 | Proceedings of 30th International GeologicalCongress1997，26，： | 1 |
| 9 | Tectonic Cha-racteristics of the Central Segment of the Tancheng -Lujiang Fault Zone, Shangdong Peninsula,EasternChina显示文摘 | Lin Aiming Miyata T Wan Tianfeng | 1998 | Tectonophysics1998，293，： | 1 |
| 10 | On Tectonogeomorphology of China显示文摘On Tectonogeomorphology of China￥WanTianfeng(DepartmentofGeologyandMineralResources,ChinaUniversityofGeosciences,Beijing10008... | Wan Tianfeng(Department of Geology and Mineral Resources, China University of Geosciences, Beijing 100083) | 1995 | Journal of Earth Science1995，14，1： | 0 |
| 11 | Magnetic Fabric of Cuizhao Pluton and ItsEmplacement Significance显示文摘The new micro-structural and magnetic fabric data on Cuizhao plutou and their emplacement implications are demonstrated in this peper. The magnetic foliations develop better and the degree of magnetic susceptibility anlsotropy is larger in the margin of the pluton than that in the center,which reveals mainly horizontal compression or magma during emplacement- The mapnetic lineations are not very well developed. The magnetic fabrics in the Cuizhao pluton reveal horizontal compression like the bollooning model during emplacement near the Earth surrace. This feature was fixed in later tectonic events. | Zhou Weixin(Institute of Geology, China Seismological Bureau, Beijing 100029)Wan Tianfeng(Department of Geology and Mineral Resources, China University of Geosciences, Beijing 100083) | 1999 | Journal of Earth Science1999，18，3： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员