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1Ages, Sources and Tectonic Settings of the Triassic Igneous Rocks in the Easternmost Segment of the East Kunlun Orogen, Central China显示文摘U–Pb analysis of zircons from igneous rocks in the Elashan Mountain, easternmost segment of the East Kunlun Orogen yielded 252–232 Ma. Geochemically, these rocks are mainly high in SiO_2, K_2O and K_2O+Na_2O contents, low in P_2O_5 and TiO_2 contents, depleted in Ba, Sr, P, Ti and enriched in U, Hf, Zr, showing features of I–type granite. The zircon εHf(t) values of the Early Triassic Jiamuge'er rhyolite porphyry(252±3 Ma) are positive(+1.6 to +12.1), suggesting a juvenile crustal source mixing with little old crustal component, and the zircon εHf(t) values of the Middle Triassic Manzhang'gang granodiorite(244±3 Ma) and Dehailong diorite(237±3 Ma) are predominately negative(-8.4 to +1.0), indicating an older crustal source. In comparison, the zircon εHf(t) values of the Late Triassic syenogranites from Suigen'ergang(234±2Ma), Ge'ermugang(233±2 Ma) and Yue'ergen(232±3 Ma) plutons vary from-3.8 to +5.0, suggesting a crust-mantle mixing source. From Early–Middle Triassic(252–237 Ma) to Late Triassic(234–232 Ma), the geochemical characteristics of these rocks show the change from a subduction–collision setting to a post-collision or within-plate setting. By comparing of these new age data with 77 zircon U–Pb ages of igneous rocks of the eastern part of East Kunlun orogen from published literatures, we conclude that the igneous rocks of Elashan Mountain and these of the eastern part of East Kunlun Orogen belong to one magmatic belt. All these data indicate that the Triassic magmatic events of the eastern part of East Kunlun Orogen can be divided into three stages: 252–238 Ma, 238–226 Ma and 226–212 Ma. Statistically, the average εHf(t) values of the threestage igneous rocks show a tendency, from the old to young, from-0.75±0.25 to lower-2.65±0.52 and then to-1.22±0.25, respectively, which reveal the change of their sources. These characteristics can be explained as a crust-mantle mixing source generated in a subductional stage, mainly crust source in a syn–collisional stage and a crust-mantle mixing source(lower crust with mantle-derived underplating magma) in a post-collisional stage. The identification of these three magmatic events in the Elashan Mountain, including all the eastern part of East Kunlun Orogen, provides new evidence for better understanding of the tectonic evolution of the northward subduction and closure of the Paleo-Tethyan(252–238 Ma), the collision of the Songpan–Ganzi block with the southern margin of Qaidam block(238–226 Ma), and the post–collisional setting(226–212 Ma) during the Early Mesozoic period.REN Haidong WANG Tao ZHANG Lei WANG Xiaoxia HUANG He FENG Chengyou TESCHNER Claudia SONG Peng 2016Acta Geologica Sinica(English Edition)2016,90,2:13
2Versatile rigid-fluid coupling for incompressible SPH显示文摘Nadir Akinci Markus Ihmsen Gizem Akinci Barbara Solenthaler Matthias Teschner 2012ACM Transactions on Graphics (TOG)2012,,4:3
3Performance, structure, and mechanism of CeO 2 in HCl oxidation to Cl 2显示文摘Amol P. Amrute Cecilia Mondelli Maximilian Moser Gerard Novell-Leruth Núria López Dirk Rosenthal Ramzi Farra Manfred E. Schuster Detre Teschner Timm Schmidt Javier Pérez-Ramírez 2011Journal of Catalysis2011,,:2
4Visual Simulation of Multiple Fluids in Computer Graphics: A State-of-the-Art Report显示文摘在多重液体之间的各种各样的相互作用的现实主义的动画,可能经历阶段变化,是在计算机图形的一项挑战性的任务。多相的多液体现象的视觉范围盖住复杂纠缠的表面结构和富有的颜色变化,它能极大地在图形应用提高视觉效果。描述如此的现象要求更复杂的模型处理包含相互作用,动力学和多重阶段的空间分发的计算的挑战,它经常被包含并且难获得即时性能。最近,算法的一个多样的集合被介绍了基于管理实现复杂多液体现象物理法律和新奇 discretization 方法到当保证时,加速全面计算数字稳定性。由在多重液体的宽广题目通过最近的研究的目标现象排序,这份最先进的报告在计算机图形在多液体模拟上总结最近的进展。Bo Ren Xu-Yun Yang Ming C. Lin Nils Thuerey Matthias Teschner Chenfeng Li 2018Journal of Computer Science & Technology2018,33,3:2
5Leflunomide: a drug with a potential beyond rheurnatology 显示文摘Teschner S Burst V 2010Immunotherapy2010,2,5:1
6Mid Frequency Sputtering-a Novel Tool for Large Area Coating显示文摘Br~uer G Szczyrbowski J Teschner G 0,,:1
7Direct forcing for Lagrangian rigid-fluid coupling 显示文摘BECKER M TESSENDORF H TESCHNER M 2008IEEE Transactions on Visual- ization and Computer Graphics2008,15,3:1
8Computer-aided 3-D simulation and prediction of craniofacial surgery: A new approach 显示文摘Girod S Teschner M Schrell U 2001J Cranio Maxillofac Surg2001,29,3:1
9Diagnosis and treatment of prima-ry mediastinal liposarcoma 显示文摘Teschner M Lullig H 2003Pneumologie2003,57,1:1
10Diagnosis and treatment of primary mediastinal liposarcoma显示文摘Teschner M Lullig H 2003Pneumologie2003,57,1:1
11Biodegradation of crude oils 显示文摘BOSECKER K TESCHNER M WEHNER H 1989Schriftenr Vet Wasser Boden Lufihyg1989,80,:1
12Meshless deformations based on shape matching显示文摘MUELLER M HEIDELBERGER B TESCHNER M 2005ACM Trans Graph2005,24,3:1
13A State Machine for Real-Tune Cutting of Tetrahedral Meshes 显示文摘D Bielser P Glardon M Teschner M Gross 2004Graphical Models (S1524-0703)2004,,66:1
14Leflunomide: a drug with a potential beyond rheumatology 显示文摘Teschner S Burst V 2010lmmunotherapy2010,2,:1
15Alcohol abuse:potential role in electrolyte disturbances and kidney diseases显示文摘Vamvakas S Teschner M Bahner U 1998Clin Nephrol1998,49,4:1
16Characterization of leakage activity in exudative chorioretinal disease with threedi- mensional confocal angiography 显示文摘Teschner S Noack J Bimgruber R 2003Ophthalmology2003,110,4:1
17Alcohol abuse:potential role in electrolyte disturbances and kidney diseases显示文摘Vamvakas S Teschner M Bahner U 1998Clin Nephrol1998,49,4:1
18Petrography, inorganic and organic geochemistry of Lower Permian carbonaceous fan sequences (' Brandschiefer Series ')-Federal Republic of Germany:constraints to their palaeogeography and assessment of their source rock potential 显示文摘DILL H TESCHNER M WEHNER H 1988Chemical Geology1988,67,:1
19Interaction of fluids with deformable solids 显示文摘MUELLER M SCHIRM S TESCHNER M 2004Comput Animat Virtual Worlds2004,15,34:1
20显示文摘Brauer G Szczyrbowski J Teschner G 1997Surface and Coating Technology1997,9495,:1
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