Origin of chalcedony nodules in rhyolite from the Peloncillo Mountains, Hidalgo County, New Mexico

P. J. Modreski
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Abstract

A particularly intriguing occurrence of chalcedony nodules has recently been recognized in mid-Tertiary silicic volcanic rocks near the Arizona-New Mexico border in southwestern Hidalgo County, New Mexico. The occurrence is in the vicinity of Clanton Draw and Geronimo Pass, in the Coronado National Forest. The nodules formed within a late Oligocene, high-silica rhyolite lava flow (Rhyolite of Clanton Draw) along the north margin of the Geronimo Trail cauldron (McIntyre, 1988; Erb, 1979; and Charles Bryan, personal communication, 1995).
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新墨西哥州伊达尔戈县Peloncillo山脉流纹岩中玉髓结核的起源
最近,在新墨西哥州西南部伊达尔戈县亚利桑那州-新墨西哥州边界附近的中第三纪硅质火山岩中发现了一种特别有趣的玉髓结核。事故发生在科罗纳多国家森林的克兰顿山口和杰罗尼莫山口附近。结核形成于晚渐新世,高硅流纹岩熔岩流(克兰顿拉流纹岩)沿杰罗尼莫径坩埚北缘(McIntyre, 1988;Erb, 1979;查尔斯·布莱恩,《个人沟通》,1995年)。
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