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Publikováno v:
Journal of South American Earth Sciences. 7:167-177
K-Ar and 40Ar/39Ar dating of volcanic rocks from the Maricunga belt of north-central Chile indicate that igneous activity took place throughout most of Miocene time at various places in the 150 by 30 km belt. No migration patterns of volcanism appear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4aa4b2bc80bdefde5a7aa22b7b5f8b0
https://doi.org/10.1016/0895-9811(94)90006-x
https://doi.org/10.1016/0895-9811(94)90006-x
The structural framework of Pahute Mesa, nevada, is dominated by the Silent Canyon caldera complex, a buried, multiple collapse caldera complex. Using the boundary surface between low density Tertiary volcanogenic rocks and denser granitic and weakly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0dccb4b3b4f2e6cab1234610d52c9bbc
https://doi.org/10.2172/15123
https://doi.org/10.2172/15123
Ground-water flow through the region south and west of Frenchman Flat, in the Ash Meadows subbasin of the Death Valley ground-water flow system, is controlled mostly by faults which arrange the distribution of permeable and impermeable rocks. In addi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42815ec0e5162098ac947366e5626ced
https://doi.org/10.2172/1713
https://doi.org/10.2172/1713
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07ad440a116e27c410f55a5acb75827c
https://doi.org/10.3133/ofr98496
https://doi.org/10.3133/ofr98496
Autor:
E.H. McKee
Publikováno v:
Open-File Report.
Ground water flow through the region south and west of Frenchman Flat, in the Ash Meadows subbasin of the Death Valley ground water flow system, is controlled mostly by the distribution of permeable and impermeable rocks. Geologic structures such as
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cce173b7305c7512a050a0c9a927e7b9
https://doi.org/10.3133/ofr97734
https://doi.org/10.3133/ofr97734
Autor:
C.G. Cunningham, Hugo Aparicio N., Fernando Murillo S., Nestor C. Jimenez, J. L. Lizeca B., E.H. McKee, G.E. Ericksen, Tavera V. Franz
Publikováno v:
Open-File Report.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e8c3651634c8c3bef062f5bfd1c8a3bc
https://doi.org/10.3133/ofr94238
https://doi.org/10.3133/ofr94238
Publikováno v:
Marine Geology. 54:M1-M8
New K-Ar ages for 13 samples of basalt, gabbro, wehrlite, and trachyandesite drilled from the Brazilian continental shelf and coastline yield information about the timing of the opening of the South Atlantic and the nature of the crust seaward from t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db6584b130798816dcb85d58cb6052b4
https://doi.org/10.1016/0025-3227(83)90002-6
https://doi.org/10.1016/0025-3227(83)90002-6
Publikováno v:
Journal of South American Earth Sciences. 2:343-349
We evaluated 193 K-Ar ages (10 newly determined) of basaltic and differentiated rocks of the Serra Geral (Parana) flood-basalt province for indications of magmatism occurring systematically with progressive rifting and complete separation ( ≈130-10
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62a7794df99c6d96936cbc6d8f6a817a
https://doi.org/10.1016/0895-9811(89)90012-6
https://doi.org/10.1016/0895-9811(89)90012-6