| 1 | Dating of the Karakorum Strike-slip Fault显示文摘This paper mainly discusses the timing of the Karakorum strike-slip fault, and gives a brief introduction of its structures, offset, and deformational style. This fault strikes NNW-SSE. Asymmetrical folds, stretching lineation, S-C fabrics, feldspar and quartz (-porphyroclasts, domino structure, shear cleavages and faults in the fault zone are products of tectonic movements. They all indicate a dextral slip sense of faulting. Mylonitic bands are widely developed along this fault. Phengite appears, indicating rather high deformational pressure. Geochronological data indicate that the Karakorum strike-slip faulting occurred from 6.88(0.36 to 8.75(0.25 Ma. The cumulative displacement from Muztag Ata to Muji is about 135 km. | ZHOU Yong, XU Ronghua, YAN Yuehua, PAN Yusheng,Tsanyao Frank YANG, Wei LO and WU Chunming Laboratory of Lithosphere Tectonic Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029Department of Geology, National Taiwan University, 245 Choushan Road, Taipei 106-17, TaiwanDepartment of Geology, Chinese Culture University, Hwa-kang, Yang-Ming-Shan, Taipei, Taiwan Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037 | 2001 | Acta Geologica Sinica(English Edition)2001，75，1： | 12 |
| 6 | 台湾─吕宋弧北部火山岩径迹年代测定:喷发年代和地壳混染证据显示文摘响应南中国海板块俯冲于西菲律宾海板块下面形成的台湾-吕宋弧的北部现在正在与欧亚大陆板块碰撞(图1)。该弧的北部早已增生到大陆边缘,导致形成了台湾东部的海岸山脉,在那里所有火山活动已停止(Teng,1990)。在它的南端,此弧已与北巴拉望-民都洛陆区相碰,而俯冲作用和相关的岩浆作用在两碰撞带之间的区段内继续着。这种空间构造背景为研究与俯冲作用和弧-陆之间碰撞有关的岩浆活动提供了理想的地方。 本文讨论的是碰撞带北部。该区的火山岩喷发年代在过去已通过一些方法研究过。已获得了29.7~0.14Ma的K-Ar年代、9.4~0.9Ma的Rb-Sr矿物等时线年代,16.0~1.1Ma的Ar-Ar年代。在使用这些方法时有某些假设,即:残留的Ar没有问题,所研究的样品的初始同位素均匀和喷发后有封闭的系统同位素演化。然而,Lan等(1986)和Chen(1989) | Tsanyao F.yang 费海德 | 1996 | 海洋地质译丛1996，，1： | 0 |
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