首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Exhumation of an accretionary prism - results from fission track thermochronology of the Shimanto Belt, southwest Japan
【24h】

Exhumation of an accretionary prism - results from fission track thermochronology of the Shimanto Belt, southwest Japan

机译:增生棱镜的发掘-日本西南部四万十地带的裂变径迹热年代学结果

获取原文
获取原文并翻译 | 示例
       

摘要

The along-are variation of the thermal history of the Shimanto accretionary prism was studied with fission track thermochronology to investigate tectonic factors that control the exhumation of an accretionary prism. Twelve apatite and 35 zircon ages were analyzed on sandstone and granite samples from the Kii and Kyushu regions. southwest Japan, and the samples are interpreted in combination with the previously reported data from the Shikoku region. Zircon samples show various degrees of age resetting after deposition that are dependent on their position within the prism. Some of the zircon samples constrain the time of maximum heating within or cooling through the zircon partial annealing zone. Two lines of observation, i.e. simultaneous exhumation revealed along across-are transect with relatively high maximum burial at the rear part of the prism, and along-are coeval rebound from burial to exhumation, indicate that the exhumation of the entire wedge was probably caused by a progressive accretionary process such as underplating at depth. Because the driving force for this type of exhumation is the growth of the wedge, this exhumation process is probably a general exhumation process that occurs in all accretionary complexes. Apatite samples record cooling at similar to 10 Ma except for samples from sites in the north of the Kii region whose ages are similar to 35 Ma, suggesting the effect of the southwest japan block obduction onto the subducting young Philippine Sea Plate. This implies, along with the distribution of locally reset zircon ages, that the exhumation of the prism was also forced by local episodic events, for example, collision of blocks during differential rotational movement, change of the subduction parameters, and possible accelerated underplating beneath a narrow region probably caused by the increased material influx from the igneous activities. (C) 2001 Elsevier Science B.V. All rights reserved. [References: 84]
机译:利用裂变径迹热年代学研究了Shimanto增生棱镜的热历史沿线变化,以研究控制增生棱镜掘出的构造因素。在来自纪伊和九州地区的砂岩和花岗岩样品上分析了十二个磷灰石和35个锆石年龄。日本西南部,并结合以前报道的四国地区数据对这些样品进行解释。锆石样品在沉积后显示出不同程度的老化时间,这取决于它们在棱镜中的位置。一些锆石样品限制了在锆石部分退火区内或通过锆石部分退火区的最大加热时间。两条观察线,即在棱柱后部沿横断面同时发掘出最大埋葬量较高的沿横断面,以及沿埋葬到掘出尸体的沿回骨期回弹,均表明整个楔形物的挖出可能是由于渐进的增生过程,例如深埋。因为这种挖掘尸体的驱动力是楔子的增长,所以这个挖掘尸体的过程很可能是在所有增生复合体中发生的一般挖掘尸体的过程。磷灰石样品记录的冷却时间约为10 Ma,除了来自纪伊地区北部的年龄约35 Ma的地点的样品外,这表明日本西南部块状引诱对俯冲的年轻菲律宾海板块的影响。这意味着,随着局部复位锆石年龄的分布,棱镜的掘出也受到局部事件的推动,例如,在不同的旋转运动过程中,块体发生碰撞,俯冲参数的变化以及可能在加速器下方的加速镀覆。火成岩活动引起的物质流入增加可能是造成狭窄区域的原因。 (C)2001 Elsevier Science B.V.保留所有权利。 [参考:84]

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号