Marius Hills火山高原位于月球正面风暴洋区域,具有丰富的火山建造遗迹,包括火山穹窿,火山锥和月溪等.该区域保留了月海火山作用的典型特征,为研究月海热演化历史提供了有利的窗口.受以往观测数据类型的限制,大多数研究都是针对该区域...Marius Hills火山高原位于月球正面风暴洋区域,具有丰富的火山建造遗迹,包括火山穹窿,火山锥和月溪等.该区域保留了月海火山作用的典型特征,为研究月海热演化历史提供了有利的窗口.受以往观测数据类型的限制,大多数研究都是针对该区域的表面形貌和物质成分特性的分析,缺乏对月海火山次表层和内部结构等重要火山特征的研究.本文利用月球正面高分辨率地形和重力数据,结合附加表面和内部载荷的弹性薄壳均衡模型,对该火山区域的平均月壳密度,岩石圈弹性厚度和表面内部载荷比等参数进行定量约束.结果显示该区域月壳密度较高,为3040 kg m 3,具有典型的月海玄武质的密度特征;地下可能存在侵位较浅的岩浆房或岩床状侵入体或是岩浆充填了壳层松散的区域;该区域的岩石圈弹性厚度较小,约为4 km,反映该区域在形成过程中富集了大量的热,该结果与通过光谱矿物分析得到的风暴洋区域富集产热元素(如钍)的结果一致.展开更多
Marius Hills is a volcanic plateau on the nearside of the Moon. It is of great interest for its high concentration of volcanic features, including domes, cones, ridges, and rilles. However, the morphological and chron...Marius Hills is a volcanic plateau on the nearside of the Moon. It is of great interest for its high concentration of volcanic features, including domes, cones, ridges, and rilles. However, the morphological and chronological characteristics of this plateau were not well studied due to the low resolution of early mission data. This study describes the detailed morphology of the volcanic features using the latest high spatial resolution images of the Terrain Camera （TC） onboard Selene-1 （10 m/pix） and Narrow Angle Camera （NAC） onboard the Lunar Reconnaissance Orbiter （LRO） （0.5 m/pix）. We report here some new structures such as skylights and remnants of lava tubes. We have divided spectrally homogenous areas with Clementine UVVIS data and did crater size frequency distribution （CSFD） measurements with Lunar Orbiter （LO） IV and TC images in every spectral unit. We first report absolute model ages of 1.10 Ga for Marius basalt 1, 1.49 Ga for Fiamsteed basalt, and 1.46 Ga for Schiaparelli Basalt. In addition, we have identified several younger lava events： they are Marius basalt 2 （814 Ma）, medium to low titanium basalt （949 Ma）, and undifferentiated medium titanium basalt （687 Ma）. Finally, we propose a mantle plume scenario for the formation of Marius Hills, which could solve the inconsistency of previous models.展开更多
Rome was famous because of its strong military force and it dominate the Mediterranean Sea.However,it was facing severe shortage of soldiers for a long time during 150 BCE.This problem had enormously effect on the Rom...Rome was famous because of its strong military force and it dominate the Mediterranean Sea.However,it was facing severe shortage of soldiers for a long time during 150 BCE.This problem had enormously effect on the Roman society and political life such as the appearance of slavery in Rome and the use of violence in Rome.The reasons why Rome had shortage f soldiers were related to its own military system and political system.The three great reformers,Tiberius Gracchus,Caius Gracchus and Caius Marius tried their best to solve the problem.Gracchus brothers failed but Marius succeed.Experiences we can learn from these reforms will also be mentioned.展开更多
文摘Marius Hills火山高原位于月球正面风暴洋区域,具有丰富的火山建造遗迹,包括火山穹窿,火山锥和月溪等.该区域保留了月海火山作用的典型特征,为研究月海热演化历史提供了有利的窗口.受以往观测数据类型的限制,大多数研究都是针对该区域的表面形貌和物质成分特性的分析,缺乏对月海火山次表层和内部结构等重要火山特征的研究.本文利用月球正面高分辨率地形和重力数据,结合附加表面和内部载荷的弹性薄壳均衡模型,对该火山区域的平均月壳密度,岩石圈弹性厚度和表面内部载荷比等参数进行定量约束.结果显示该区域月壳密度较高,为3040 kg m 3,具有典型的月海玄武质的密度特征;地下可能存在侵位较浅的岩浆房或岩床状侵入体或是岩浆充填了壳层松散的区域;该区域的岩石圈弹性厚度较小,约为4 km,反映该区域在形成过程中富集了大量的热,该结果与通过光谱矿物分析得到的风暴洋区域富集产热元素(如钍)的结果一致.
基金supported by the National Natural Science Foundation of China (Nos. 41072045, 41102209)the Research Fund for the Doctoral Program of Higher Education (No. 20090145110001)+1 种基金Nondestructive Analysis Technique and Best Analysis Scheme of Lunar Sample (No. TY3Q20110029)China University of Geosciences (Wuhan) GF Special Research Fund (No. CUGXGF0901)
文摘Marius Hills is a volcanic plateau on the nearside of the Moon. It is of great interest for its high concentration of volcanic features, including domes, cones, ridges, and rilles. However, the morphological and chronological characteristics of this plateau were not well studied due to the low resolution of early mission data. This study describes the detailed morphology of the volcanic features using the latest high spatial resolution images of the Terrain Camera （TC） onboard Selene-1 （10 m/pix） and Narrow Angle Camera （NAC） onboard the Lunar Reconnaissance Orbiter （LRO） （0.5 m/pix）. We report here some new structures such as skylights and remnants of lava tubes. We have divided spectrally homogenous areas with Clementine UVVIS data and did crater size frequency distribution （CSFD） measurements with Lunar Orbiter （LO） IV and TC images in every spectral unit. We first report absolute model ages of 1.10 Ga for Marius basalt 1, 1.49 Ga for Fiamsteed basalt, and 1.46 Ga for Schiaparelli Basalt. In addition, we have identified several younger lava events： they are Marius basalt 2 （814 Ma）, medium to low titanium basalt （949 Ma）, and undifferentiated medium titanium basalt （687 Ma）. Finally, we propose a mantle plume scenario for the formation of Marius Hills, which could solve the inconsistency of previous models.
文摘Rome was famous because of its strong military force and it dominate the Mediterranean Sea.However,it was facing severe shortage of soldiers for a long time during 150 BCE.This problem had enormously effect on the Roman society and political life such as the appearance of slavery in Rome and the use of violence in Rome.The reasons why Rome had shortage f soldiers were related to its own military system and political system.The three great reformers,Tiberius Gracchus,Caius Gracchus and Caius Marius tried their best to solve the problem.Gracchus brothers failed but Marius succeed.Experiences we can learn from these reforms will also be mentioned.
