首页> 美国政府科技报告 >MAJOR-ELEMENT GEOCHEMISTRY OF THE SILENT CANYON-BLACK MOUNTAIN PERALKALINE VOLCANIC CENTERS, NORTHWESTERN NEVADA TEST SITE: APPLICATIONS TO AN ASSESSMENT OF RENEWED VOLCANISM
【24h】

MAJOR-ELEMENT GEOCHEMISTRY OF THE SILENT CANYON-BLACK MOUNTAIN PERALKALINE VOLCANIC CENTERS, NORTHWESTERN NEVADA TEST SITE: APPLICATIONS TO AN ASSESSMENT OF RENEWED VOLCANISM

机译:内华达西北部测试场地沉默的黑色山脉 - 黑色火山岩火山中心的主要元素地球化学:应用于评估更新的火山活动

获取原文

摘要

The Silent Canyon and Black Mountain volcanic centers are located in the northern part of the Nevada Test Site. The Silent Canyon volcanic center is a buried cauldron complex of Miocene age (13-15 m.y.). Black Mountain volcanic center is an elliptical-shaped cauldron complex of late Miocene age.nThe lavas and tuffs of the two centers comprise a subalkaline-peralkaline association. Rock types range from quartz normative subalkaline tracheae and hyalite to peralkaline comedies. The Gold Flat Member of the Thirsty Canyon Tuff (Black Mountain) is a pantellerite.

著录项

相似文献

  • 外文文献
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