Zobrazeno 1 - 9
of 9
pro vyhledávání: '"C. H. Simonds"'
Autor:
C. H. Simonds, Susan W. Kieffer
Publikováno v:
Journal of Geophysical Research: Solid Earth. 98:14321-14337
The controversy that raged through the 1950s to 1970s over similarities and differences between meteorite impact and volcanic processes is revisited. We propose that there are quantitative similarities in erosion caused by high-speed ejecta produced
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bac60d3cbf3a517d0e6db64822e07c01
https://doi.org/10.1029/93jb00704
https://doi.org/10.1029/93jb00704
Autor:
G. W. Pearce, C. H. Simonds
Publikováno v:
Journal of Geophysical Research. 79:2953-2959
The Apollo 16 crystalline rocks have a greater average percentage of metallic iron than any other lunar material and are the most reduced in terms of their metallic iron/total iron ratio. They have greater metal content than the mare basalts, the onl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b22a29786672d855cea85659194c72c5
https://doi.org/10.1029/jb079i020p02953
https://doi.org/10.1029/jb079i020p02953
Autor:
R. J. Floran, C. H. Simonds, M. R. Dence, J. L. Warner, W. C. Phinney, R. A. F. Grieve, M. J. Rhodes, Bor-ming Jahn
Publikováno v:
Geophysical Research Letters. 3:49-52
Chemical, petrographic, isotopic and field studies of igneous-textured rocks within the Manicouagan structure indicate that they are the product of impact melting. Features of the melt sheet include a high degree of textural variation combined with c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee7e3392003dcf6e88713cdf88346aaf
https://doi.org/10.1029/gl003i002p00049
https://doi.org/10.1029/gl003i002p00049
Publikováno v:
Journal of Geophysical Research. 83:2773
It is suggested, on the basis of previous theoretical studies of shock waves, that the Manicouagan melt formed in 1 or 2 s in a 5-km-radius hemisphere near the point of impact. The melt and the less shocked debris surrounding it flowed downward and o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46586c8b76bdce26ca4fdcd16c48d795
https://doi.org/10.1029/jb083ib06p02773
https://doi.org/10.1029/jb083ib06p02773
Publikováno v:
Geophysical Research Letters. 10:599-599
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::715b55b6d431139a93f6eb4236f2607d
https://doi.org/10.1029/gl010i007p00599
https://doi.org/10.1029/gl010i007p00599
Autor:
Susan W. Kieffer, C. H. Simonds
Publikováno v:
Reviews of Geophysics. 18:143
A survey of published descriptions of 32 of the largest, least eroded terrestrial impact structures shows that the amount of melt at craters in crystalline rocks is approximately two orders of magnitude greater than that at craters in sedimentary roc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::950fa47b456a3f17656487fefed68a7c
https://doi.org/10.1029/rg018i001p00143
https://doi.org/10.1029/rg018i001p00143
Publikováno v:
Journal of Geophysical Research. 83:2799
Rb-Sr isotopic data for mineral separates from a rock of the Manicouagan impact melt sheet define an isochron of age T = 214 + or - 5 (2 sigma) m.y. which agrees with the K-Ar age of 210 + or - 8 (2 sigma) calculated by Wolfe (1971). The initial Sr-8
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aacdd0eaced40cef63849a8aa3153c38
https://doi.org/10.1029/jb083ib06p02799
https://doi.org/10.1029/jb083ib06p02799
Publikováno v:
Journal of Geophysical Research. 83:2789
Calculations for the heat transfer between superheated silicate melt and evenly dispersed 1-mm cold clasts indicate that most of the thermal gradients are smoothed out in 100 s and that the rate of equilibrium is sufficiently high so that clasts whos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a787802d9d68afa601ebfcfc3c277a6c
https://doi.org/10.1029/jb083ib06p02789
https://doi.org/10.1029/jb083ib06p02789