Several Geological Issues of Schrodinger Basin Exposed by CE-2 CELMS Data

被引：5

作者：

Meng, Z. G. ^{[1
,2
,3
]}

Wang, H. H. ^{[1
]}

Zheng, Y. C. ^{[3
]}

Wang, Y. Z. ^{[1
]}

Miyamoto, H. ^{[4
]}

Cai, Z. C. ^{[2
]}

Ping, J. S. ^{[3
]}

Zhu, Y. Z. ^{[1
]}

机构：

[1] Jilin Univ, Coll Geoexplorat Sci & Technol, Changchun 130026, Jilin, Peoples R China

[2] Macau Univ Sci & Technol, State Key Lab Lunar & Planetary Sci, Macau, Peoples R China

[3] Chinese Acad Sci, Key Lab Lunar & Deep Space Explorat, Natl Astron Observ, Beijing 100101, Peoples R China

[4] Univ Tokyo, Univ Museum, Bunkyo Ku, Tokyo 1130033, Japan

来源：

ADVANCES IN ASTRONOMY | 2019年 / 2019卷

基金：

中国国家自然科学基金;

关键词：

MICROWAVE BRIGHTNESS TEMPERATURE; SURFACE TEMPERATURE; MOON; INSIGHTS;

D O I：

10.1155/2019/3926082

中图分类号：

P1 [天文学];

学科分类号：

0704 ;

摘要：

The study on the Schrodinger basin may provide important clues about the formation of South Pole-Aitken (SPA) basin. In this paper, the thermophysical features of Schrodinger basin were evaluated using the Chang'E-2 microwave sounder (CELMS) data. The results are as follows. (1) The geological units are reevaluated with the CELMS data and a new geological view was provided according to the brightness temperature and emissivity maps. (2) The surface topography plays an important role in the observed CELMS data. (3) The hot anomaly in the basin floor indicates a warm substrate. (4) The pyroxene-bearing anorthosite is probably an important cause for the cold anomaly over the lunar surface. Also, the study proves the applicability of the CELMS data applying in high latitude regions to a certain extent.

引用

页数：13