Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Martha M. Godchaux"'
Publikováno v:
Bulletin of Volcanology. 70:315-342
New 40Ar-39Ar geochronology, bulk rock geochemical data, and physical characteristics for representative stratigraphic sections of rhyolite ignimbrites and lavas from the west-central Snake River Plain (SRP) are combined to develop a coherent stratig
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6186b0a1ac4178f799a4276129011895
https://doi.org/10.1007/s00445-007-0141-6
https://doi.org/10.1007/s00445-007-0141-6
Publikováno v:
Bulletin of Volcanology. 66:485-491
Structural reappraisal of several classic rheomorphic ignimbrites in Colorado, Idaho, the Canary Islands and Italy has, for the first time, revealed abundant oblique folds, curvilinear folds and sheathfolds which formed during emplacement. Like their
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9685d39dae77d7ef9f9acade0181613c
https://doi.org/10.1007/s00445-003-0332-8
https://doi.org/10.1007/s00445-003-0332-8
Autor:
Gerardo J. Aguirre-Díaz, Luis Fernando Vassallo-Morales, Martha M. Godchaux, Pablo Dávila-Harris, Bill Bonnichsen, Maria Amabel Ortega-Rivera, José Jorge Aranda-Gómez, Juventino Martínez-Reyes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7dc278f0c232654fa9e7c1bd9deeafe9
https://doi.org/10.1130/2012.0025(07)
https://doi.org/10.1130/2012.0025(07)
Publikováno v:
Journal of Volcanology and Geothermal Research. 52:1-25
The western Snake River Plain graben in southwestern Idaho includes a large hydrovolcanic field which was produced in late Miocene to Pleistocene time by the interaction of rising basaltic magmas with the waters and water-saturated deposits of an eno
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0758594e1623482d7a75a27cf3dfdaf
https://doi.org/10.1016/0377-0273(92)90130-6
https://doi.org/10.1016/0377-0273(92)90130-6
Publikováno v:
Geology. 33:821
The Miocene Bruneau-Jarbidge and adjacent volcanic fields of the central Snake River Plain, southwest Idaho, are dominated by high-temperature rhyolitic tuffs and lavas having an aggregate volume estimated as 7000 km3. Samples from units representing
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8048d8be7ecdc67bda6377d50a982ed0
https://doi.org/10.1130/g21723.1
https://doi.org/10.1130/g21723.1