NEAR at Eros: Imaging and spectral results

被引:221
作者
Veverka, J
Robinson, M
Thomas, P
Murchie, S
Bell, JF
Izenberg, N
Chapman, C
Harch, A
Bell, M
Carcich, B
Cheng, A
Clark, B
Domingue, D
Dunham, D
Farquhar, R
Gaffey, MJ
Hawkins, E
Joseph, J
Kirk, R
Li, H
Lucey, P
Malin, M
Martin, P
McFadden, L
Merline, WJ
Miller, JK
Owen, WM
Peterson, C
Prockter, L
Warren, J
Wellnitz, D
Williams, BG
Yeomans, DK
机构
[1] Cornell Univ, Ithaca, NY 14853 USA
[2] Northwestern Univ, Dept Geol Sci, Evanston, IL 60208 USA
[3] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD 20723 USA
[4] SW Res Inst, Boulder, CO 80302 USA
[5] Rensselaer Polytech Inst, Ctr Sci, Dept Earth & Environm Sci, Troy, NY 12180 USA
[6] US Geol Survey, Flagstaff, AZ 86001 USA
[7] Univ Hawaii, Hawaii Inst Geophys & Planetol, Honolulu, HI 96822 USA
[8] Malin Space Sci Syst, San Diego, CA 92191 USA
[9] Univ Maryland, Dept Astron, College Pk, MD 20742 USA
[10] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
关键词
D O I
10.1126/science.289.5487.2088
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Eros is a very elongated (34 kilometers by 11 kilometers by 11 kilometers) asteroid, most of the surface of which is saturated with craters smaller than 1 kilometer in diameter. The Largest crater is 5.5 kilometers across, but there is a 10-kilometer saddle-like depression with attributes of a large degraded crater. Surface Lineations, both grooves and ridges, are prominent on Eros; some probably exploit planes of weakness produced by collisions on Ems and/or its parent body. Ejecta blocks (30 to 100 meters across) are abundant but not uniformly distributed over the surface. Albedo variations are restricted to the inner walls of certain craters and may be related to downslope movement of regolith. On scales of 200 meters to 1 kilometer, Eros is more bland in terms of color variations than Gaspra or Ida. Spectra (800 to 2500 nanometers) are consistent with an ordinary chondrite composition for which the measured mean density of 2.67 +/- 0.1 grams per cubic centimeter implies internal porosities ranging from about 10 to 30 percent.
引用
收藏
页码:2088 / 2097
页数:10
相关论文
共 61 条
[1]   SPECTRAL REFLECTANCE 0.4 TO 2.0 MICRONS OF SILICATE ROCK POWDERS [J].
ADAMS, JB ;
FILICE, AL .
JOURNAL OF GEOPHYSICAL RESEARCH, 1967, 72 (22) :5705-+
[2]   Mechanical and geological effects of impact cratering on Ida [J].
Asphaug, E ;
Moore, JM ;
Morrison, D ;
Benz, W ;
Nolan, MC ;
Sullivan, RJ .
ICARUS, 1996, 120 (01) :158-184
[3]   The discovery and orbit of 1993 (243)1 Dactyl [J].
Belton, MJS ;
Mueller, BEA ;
DAmario, LA ;
Byrnes, DV ;
Klaasen, KP ;
Synnott, S ;
Breneman, H ;
Johnson, TV ;
Thomas, PC ;
Veverka, J ;
Harch, AP ;
Davies, ME ;
Merline, WJ ;
Chapman, CR ;
Davis, D ;
Denk, T ;
Neukum, G ;
Petit, JM ;
Greenberg, R ;
Storrs, A ;
Zellner, B .
ICARUS, 1996, 120 (01) :185-199
[4]   On a possible rotation state of (433) Eros [J].
Black, GJ ;
Nicholson, PD ;
Bottke, WF ;
Burns, JA ;
Harris, AW .
ICARUS, 1999, 140 (01) :239-242
[5]   THE GEOLOGY OF GASPRA [J].
CARR, MH ;
KIRK, RL ;
MCEWEN, A ;
VEVERKA, J ;
THOMAS, P ;
HEAD, JW ;
MURCHIE, S .
ICARUS, 1994, 107 (01) :61-71
[6]   SURFACE PROPERTIES OF ASTEROIDS - SYNTHESIS OF POLARIMETRY, RADIOMETRY, AND SPECTROPHOTOMETRY [J].
CHAPMAN, CR ;
MORRISON, D ;
ZELLNER, B .
ICARUS, 1975, 25 (01) :104-130
[7]   Cratering on Mathilde [J].
Chapman, CR ;
Merline, WJ ;
Thomas, P .
ICARUS, 1999, 140 (01) :28-33
[8]   J,H,K PHOTOMETRY OF 433-EROS AND OTHER ASTEROIDS [J].
CHAPMAN, CR ;
MORRISON, D .
ICARUS, 1976, 28 (01) :91-94
[9]   Cratering on Gaspra [J].
Chapman, CR ;
Veverka, J ;
Belton, MJS ;
Neukum, G ;
Morrison, D .
ICARUS, 1996, 120 (01) :231-245
[10]   Cratering on Ida [J].
Chapman, CR ;
Ryan, EV ;
Merline, WJ ;
Neukum, G ;
Wagner, R ;
Thomas, PC ;
Veverka, J ;
Sullivan, RJ .
ICARUS, 1996, 120 (01) :77-86