Fate of outflow channel effluents in the northern lowlands of Mars: The Vastitas Borealis Formation as a sublimation residue from frozen ponded bodies of water
about
Tsunami waves extensively resurfaced the shorelines of an early Martian ocean.Martian outflow channels: How did their source aquifers form, and why did they drain so rapidly?MARSIS radar sounder evidence of buried basins in the northern lowlands of Mars.Late Hesperian to early Amazonian midlatitude Martian valleys: Evidence from Newton and Gorgonum basinsDielectric map of the Martian northern hemisphere and the nature of plain filling materialsAncient oceans in the northern lowlands of Mars: Evidence from impact crater depth/diameter relationshipsModeling tsunami propagation and the emplacement of thumbprint terrain in an early Mars ocean
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P2860
Fate of outflow channel effluents in the northern lowlands of Mars: The Vastitas Borealis Formation as a sublimation residue from frozen ponded bodies of water
description
2002 nî lūn-bûn
@nan
2002 թուականի Դեկտեմբերին հրատարակուած գիտական յօդուած
@hyw
2002 թվականի դեկտեմբերին հրատարակված գիտական հոդված
@hy
2002年の論文
@ja
2002年論文
@yue
2002年論文
@zh-hant
2002年論文
@zh-hk
2002年論文
@zh-mo
2002年論文
@zh-tw
2002年论文
@wuu
name
Fate of outflow channel efflue ...... frozen ponded bodies of water
@ast
Fate of outflow channel efflue ...... frozen ponded bodies of water
@en
type
label
Fate of outflow channel efflue ...... frozen ponded bodies of water
@ast
Fate of outflow channel efflue ...... frozen ponded bodies of water
@en
prefLabel
Fate of outflow channel efflue ...... frozen ponded bodies of water
@ast
Fate of outflow channel efflue ...... frozen ponded bodies of water
@en
P2860
P3181
P356
P1476
Fate of outflow channel efflue ...... frozen ponded bodies of water
@en
P2860
P304
P3181
P356
10.1029/2001JE001831
P407
P577
2002-12-01T00:00:00Z