Imaging of volcanic activity on Jupiter's moon Io by Galileo during the Galileo Europa Mission and the Galileo Millennium Mission

L. Keszthelyi, A. S. McEwen, C. B. Phillips, M. Milazzo, P. Geissler, E. P. Turtle, J. Radebaugh, D. A. Williams, D. P. Simonelli, H. H. Breneman, K. P. Klaasen, G. Levanas, T. Denk, D. D.A. Alexander, K. Capraro, S. H. Chang, A. C. Chen, J. Clark, D. L. Conner, A. CulverT. H. Handley, D. N. Jensen, D. D. Knight, S. K. LaVoie, M. McAuley, V. Mego, O. Montoya, H. B. Mortensen, S. J. Noland, R. R. Patel, T. M. Pauro, C. L. Stanley, D. J. Steinwand, T. F. Thaller, P. J. Woncik, G. M. Yagi, J. R. Yoshimizu, E. M. Alvarez Del Castillo, M. J.S. Belton, R. Beyer, D. Branston, M. B. Fishburn, B. Mueller, R. Ragan, N. Samarasinha, C. D. Anger, C. Cunningham, B. Little, S. Arriola, M. H. Carr, E. Asphaug, J. Moore, D. Morrison, K. Rages, D. Banfield, M. Bell, J. A. Burns, B. Carcich, B. Clark, N. Currier, I. Dauber, P. J. Gierasch, P. Helfenstein, M. Mann, O. Othman, L. Rossier, N. Solomon, R. Sullivan, P. C. Thomas, J. Veverka, T. Becker, K. Edwards, L. Gaddis, R. Kirk, E. Lee, T. Rosanova, R. M. Sucharski, R. F. Beebe, A. Simon, K. Bender, F. Chuang, S. Fagents, P. Figueredo, R. Greeley, K. Homan, S. Kadel, J. Kerr, J. Klemaszewski, E. Lo, W. Schwarz, R. Sullivan, K. Williams, E. Bierhaus, S. Brooks, C. R. Chapman, B. Merline, J. Keller, P. Schenk, P. Tamblyn, A. Bouchez, U. Dyundian, A. P. Ingersoll, A. Showman, J. Spitale, S. Stewart, A. Vasavada, W. F. Cunningham, T. V. Johnson, T. J. Jones, J. M. Kaufman, K. P. Magee, M. K. Meredith, G. S. Orton, D. A. Senske, A. West, D. Winther, G. Collins, W. J. Fripp, J. W. Head, R. Pappalardo, S. Pratt, L. Procter, N. Spaun, T. Colvin, M. Davies, E. M. DeJong, J. Hall, S. Suzuki, Z. Gorjian, B. Giese, U. Koehler, G. Neukum, J. Oberst, T. Roatsch, W. Tost, P. Schuster, R. Wagner, N. Dieter, D. Durda, R. J. Greenberg, G. Hoppa, W. Jaeger, J. Plassman, R. Tufts, F. P. Fanale, J. C. Granahan, W. H. Ip, M. McElroy, J. Yatteau, W. B. Moore, G. Schubert, C. B. Pilcher

研究成果: 雜誌貢獻期刊論文同行評審

110 引文 斯高帕斯(Scopus)

摘要

The Solid-State Imaging (SSI) instrument provided the first high- and medium-resolution views of Io as the Galileo spacecraft closed in on the volcanic body in late 1999 and early 2000. While each volcanic center has many unique features, the majority can be placed into one of two broad categories. The "Promethean" eruptions, typified by the volcanic center Prometheus, are characterized by long-lived steady eruptions producing a compound flow field emplaced in an insulating manner over a period of years to decades. In contrast, "Pillanian" eruptions are characterized by large pyroclastic deposits and short-lived but high effusion rate eruptions from fissures feeding open-channel or open-sheet flows. Both types of eruptions commonly have ∼100-km-tall, bright, SO2-rich plumes forming near the flow fronts and smaller deposits of red material that mark the vent for the silicate lavas.

原文???core.languages.en_GB???
文章編號2000JE001383
頁(從 - 到)33025-33052
頁數28
期刊Journal of Geophysical Research: Planets
106
發行號E12
DOIs
出版狀態已出版 - 25 12月 2001

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