...
  • 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Journal of Volcanology and Geothermal Research2012V243-244NOCT,15 >The Acoculco Caldera Complex magmas: Genesis, evolution and relation with the Acoculco geothermal system
【24h】

The Acoculco Caldera Complex magmas: Genesis, evolution and relation with the Acoculco geothermal system

机译：Acoculco破火山口复杂岩浆：Acoculco地热系统的成因，演化及与之的关系

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

The Acoculco Caldera Complex (ACC) is located in the eastern part of the Trans-Mexican Volcanic Belt, Mexico. The ACC was formed 2.7 Ma, and since then, volcanic activity has persisted until 0.06 Ma, through the emission of domes, cinder cones, fissure lava flows and two ignimbrite eruptions dated at 1.2 and 0.65 Ma. The pervasive hydrothermal alteration in the central part of the ACC has motivated considerable geothermal exploration, however, none of it assessed the relation between the magmatic heat supply and the evolution of magmas, including their reservoir depth.
机译：Acoculco破火山口综合体（ACC）位于墨西哥跨墨西哥火山带的东部。 ACC形成于2.7 Ma，此后，通过散发圆顶，煤渣锥，裂隙熔岩流以及两次日期分别为1.2和0.65 Ma的火成岩喷发，火山活动一直持续到0.06 Ma。 ACC中部普遍的热液蚀变激发了大量的地热勘探，但是，没有一个能评估岩浆热供应与岩浆演化之间的关系，包括其储层深度。

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