...
首页> 外文期刊>Journal of geophysical research. Planets >The Lunar Mare Ring-Moat Dome Structure (RMDS) Age Conundrum: Contemporaneous With Imbrian-Aged Host Lava Flows or Emplaced in the Copernican?
【24h】

The Lunar Mare Ring-Moat Dome Structure (RMDS) Age Conundrum: Contemporaneous With Imbrian-Aged Host Lava Flows or Emplaced in the Copernican?

机译:月球母马Ring-Moat穹顶结构(限制型心肌病)时代难题:同生同Imbrian-Aged主机熔岩流或安放在哥白尼吗?

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Ring-moat dome structures (RMDSs) are small circular mounds of diameter typically about 200 m and ~3-4 m in height, surrounded by narrow, shallow moats. They occur in clusters, are widespread in ancient Imbrian-aged mare basalt host units and show mineralogies comparable to those of their host units. Based on these close associations and similarities, a model has been proposed for the formation of RMDS as the result of late-stage flow inflation, with second boiling releasing quantities of magmatic volatiles that migrate to the top of the flow as magmatic foams and extrude through cracks in the cooled upper part of the flow to produce the small RMDS domes and surrounding moats. In contrast to this model advocating a contemporaneous emplacement of RMDSs and their host lava flows, a range of observations suggests that the RMDS formed significantly after the emplacement and cooling of their host lava flows, perhaps as recently as in the Copernican Period (~1.1 Ga to the present). These observations include: (a) stratigraphic embayment of domes into post-lava flow emplacement impact craters; (b) young crater degradation age estimates for the underlying embayed craters; (c) regolith development models that predict thicknesses in excess of the observed topography of domes and moats; (d) landform diffusional degradation models that predict very young ages for mounds and moats; (e) suggestions of fewer superposed craters on the mounds than on the adjacent host lava flows, and (f) observations of superposed craters that suggest that the mound substrate does not have the properties predicted by the magmatic foam model. Together, these observations are consistent with the RMDS formation occurring during the period after the extrusion and solidification of the host lava flows, up to and including the geologically recent Late Copernican, that is, the last few hundreds of millions of years of lunar history. We present and discuss each of these contradictory data and interpretation
机译:Ring-moat穹顶结构(RMDSs)很小通常圆形成堆的直径约200米和~ 3 - 4米高,周围狭窄,肤浅的护城河。广泛的古代Imbrian-aged母马玄武岩主办单位和矿物学媲美的主办单位。协会和相似之处,一个模型提出了限制型心肌病的形成的结果晚期流的通货膨胀,与第二沸腾释放出大量的岩浆挥发物迁移到顶部流动的岩浆泡沫通过冷却上的裂缝和挤压流产生的一部分小限制型心肌病穹顶和周围的护城河。提倡一个同时代的RMDSs侵位和他们的主人熔岩流,一个范围的观测表明,限制型心肌病侵位和冷却后明显主机的熔岩流,也许就在在哥白尼(~ 1.1 Ga礼物)。地层物质湾的穹顶流侵位的撞击坑;退化年龄估计底层多湾坑;预测厚度超过观察地形的穹顶和护城河;地形扩散退化模型预测年龄非常小的聋成堆,护城河;更少的叠加陨石坑的建议比相邻的主机上的熔岩流成堆,(f)的观察叠加陨石坑建议丘衬底没有属性的预测岩浆泡沫模型。形成符合限制型心肌病发生期间在挤压和凝固的熔岩流,和包括地质最近迟到哥白尼,过去几个数百数百万年的月球的历史。并讨论这些互相矛盾的数据解释

著录项

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