Zobrazeno 1 - 10
of 128
pro vyhledávání: '"D. L. Bindschadler"'
Publikováno v:
Acta Astronautica. 53:329-352
After a six-year odyssey, Galileo has completed its survey of the large moons of Jupiter. In the four years since the end of the primary mission, Galileo provided new insights into the fundamental questions concerning Jupiter and its moons and magnet
Publikováno v:
Acta Astronautica. 53:85-122
Galileo has completed the long awaited Io flybys of the Galileo Europa Mission and the Galileo Millennium Mission, and is now pumping up its apojove in each succeeding orbit in preparation for the chance to perform a dual spacecraft observation of th
Publikováno v:
Icarus. 111:417-432
Magellan altimetry data reveal that the center of figure (CF) of Venus is displaced approximately 280 m from its center of mass (CM) toward 4.4 deg S, 135.8 deg E, a location in Aphrodite Terra. This offset is smaller than those of other terrestrial
Autor:
D. L. Bindschadler, Richard E. Young, Howard Houben, Gerald Schubert, Leonhard Pfister, Richard L. Walterscheid
Publikováno v:
Journal of the Atmospheric Sciences. 51:1857-1875
This paper extends the study of stationary gravity waves generated near the surface of Venus reported previously by Young et al. to include finite amplitude effects associated with large amplitude waves. Waves are forced near the surface of Venus by
Autor:
D. L. Bindschadler, Jeffrey E. Moersch, Gerald Schubert, Donald L. Turcotte, E. R. Stofan, Steven W. Squyres, Daniel M. Janes
Publikováno v:
Geophysical Research Letters. 20:2965-2968
Coronae are large quasi-circular geologica features that are common on Venus. They appear to be the surface tectonic and volcanic expressions of mantle diapirs that have impinged on the underside of the venusian lithosphere. We have investigated the
Publikováno v:
Geophysical Research Letters. 18:2209-2212
The origin and evolution of Ishtar Terra is modeled using numerical simulations of crust/mantle interaction on Venus. Based on our modeling, we favor a two phase evolutionary sequence for Ishtar. The first phase is driven by bulk mantle flow due to t
Publikováno v:
Geophysical Research Letters. 17:1345-1348
It is proposed that western Ishtar Terra formed due to compression and crustal thickening above a cylindrical mantle downwelling. A model for crustal deformation due to downwelling successfully reproduces many observed characteristics of western Isht
Autor:
Yu. G. Shkuratov, Alexander T. Basilevsky, James W. Head, Mikhail A. Ivanov, Mikhail A. Kreslavsky, D. L. Bindschadler
Publikováno v:
Geophysical Research Letters. 17:171-174
Tessera terrain is the dominant tectonic unit in the northern hemisphere of Venus and is characterized by complex sets of intersecting structural trends and distinctive radar properties due to a high degree of meter and sub-meter scale (5 cm to 10 m)
Publikováno v:
54th International Astronautical Congress of the International Astronautical Federation, the International Academy of Astronautics, and the International Institute of Space Law.
A summary of spacecraft performance in the harsh jovian environment and a report of final subsystem and instrument status are provided.