Zobrazeno 1 - 4
of 4
pro vyhledávání: '"J. L. Ahern"'
Publikováno v:
The Journal of Geology. 89:421-432
A mechanism is examined which allows an intrusive body to melt its way upward in the earth's crust. Due to the increase in melting temperature with depth the melt temperature at the base of an intrusion may be considerably greater than the melt tempe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f5341ca7527ce8f615cc634b60e8317a
https://doi.org/10.1086/628606
https://doi.org/10.1086/628606
Autor:
S. R. Mrkvicka, J. L. Ahern
Publikováno v:
Tectonics. 3:79-102
The Williston Basin is a large, circular, intracratonic basin containing over 4 km of sediments ranging in age from Cambrian to Tertiary. Data on seven formations from over 1300 wells in Montana, South Dakota, and North Dakota were used to determine
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f53d111ccf192616bea41410e790be79
https://doi.org/10.1029/tc003i001p00079
https://doi.org/10.1029/tc003i001p00079
Autor:
D. L. Turcotte, J. L. Ahern
Publikováno v:
Journal of Geophysical Research. 82:3762-3766
The cooling of the oceanic lithosphere causes subsidence by isostasy. This subsidence results in the formation of ocean basins. In this paper we assume that the subsiding lithosphere is covered with sediments. A similarity solution is obtained for th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::83d76b99cee0c11a551b4fe2c87993a6
https://doi.org/10.1029/jb082i026p03762
https://doi.org/10.1029/jb082i026p03762
Autor:
J. L. Ahern, D. L. Turcotte
Publikováno v:
Journal of Geophysical Research. 83:767
It is generally accepted that a large fraction of the earth's volcanism is due to pressure release melting of mantle rock in the ascending limbs of mantle convection cells. A problem that remains largely unsolved is the migration of the melt from the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81e2138ca185bf03ef86a39a1bd9fb6d
https://doi.org/10.1029/jb083ib02p00767
https://doi.org/10.1029/jb083ib02p00767