亚丁熔岩流,多阿纳县,新墨西哥州

R. Dehon, R. Earl
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摘要

亚丁火山口是位于拉斯克鲁塞斯西南约40公里处的Potrillo火山场的一个小火山盾。盾层和周围的流场被映射为火山相,其形态受熔岩流变学的支配。从火山口向东和向南延伸的流场由早期的流动玄武岩组成,这些玄武岩膨胀到不同的厚度,这取决于地壳的强度。水流膨胀形成边缘陡峭的平顶高原。该油田是膨胀高原的崎岖堆积,其中相邻的流缘形成了深沟。亚丁盾的形成是因为黏度增加,熔岩开始在火山口上积聚。盾状相由基底薄的痂状流、非常低的斜状叶状流和较陡的槽状流的上坡组成,顶部有一个宽的浅坑。197
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Aden lava flows, Do�a Ana County, New Mexico
Aden Crater is a small volcanic shield in the Potrillo Volcanic Field approximately 40 km southwest from Las Cruces. The shield and surrounding flow field are mapped as volcanic facies in which the morphology is governed by the rheology of the lava. The flow field which spreads east and south from the vent consist of early, fluid basalts that inflated to various thicknesses determined by the strength of the outer crust. Flows inflated to form steep-margined, flat-topped plateaus. The field is a rugged accumulation of inflation plateaus in which adjacent flow margins form deep intervening ravines. The Aden shield was formed as viscosity increased to the point that the lavas began to accumulate over the vent. The shield facies consist of basal thin scabby flows, very low sloping lobate flows, and an upper slope of steeper channeled flows, with a wide shallow crater at the top. 197
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