Zobrazeno 1 - 10
of 32
pro vyhledávání: '"John E. Warme"'
Autor:
John E. Warme, Jesús A. Pinto
Publikováno v:
The Mountain Geologist. 53:93-114
We interpret a discrete, anomalous ~10-m-thick interval of the shallow-marine Middle to Late Devonian Valentine Member of the Sultan Formation at Frenchman Mountain, southern Nevada, to be a seismite, and that it was generated by the Alamo Impact Eve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b75d4d90b2e55f509e82abedc92a4745
https://doi.org/10.31582/rmag.mg.53.2.93
https://doi.org/10.31582/rmag.mg.53.2.93
Autor:
John E. Warme
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f5c9d028c7ce3d73fb47206b22301a08
https://doi.org/10.1130/abs/2016am-285553
https://doi.org/10.1130/abs/2016am-285553
Publikováno v:
Meteoritics & Planetary Science. 46:919-922
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a21ee5b8ee0bf903856dc8edb176aff
https://doi.org/10.1111/j.1945-5100.2011.01208.x
https://doi.org/10.1111/j.1945-5100.2011.01208.x
Publikováno v:
The Sedimentary Record. 3:4-8
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb78d893927fe640f96306e935bbc465
https://doi.org/10.2110/sedred.2005.1.4
https://doi.org/10.2110/sedred.2005.1.4
Autor:
Hans-Christian Kuehner, John E. Warme
Publikováno v:
International Geology Review. 40:189-216
The Alamo Breccia is a carbonate rock breccia of Late Devonian age in southern Nevada. It is an anomalous sedimentary unit because it has the properties of a massive debris-flow and turbidity-current deposit that would be expected to occur in deep wa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01de3fab3b536941f48988237bee3d7c
https://doi.org/10.1080/00206819809465206
https://doi.org/10.1080/00206819809465206
Autor:
John E. Warme
Publikováno v:
The Atlas System of Morocco ISBN: 3540190864
The present Central and Eastern High Atlas mountains of southern Morocco represent a short-lived Mesozoic rift, 500 × 100 km, associated with an ancient fracture zone between the Saharan Craton to the south and the smaller microplate mesetas to the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e910e4ad0b352bbf426d79ed487bef8
https://doi.org/10.1007/bfb0011593
https://doi.org/10.1007/bfb0011593
Publikováno v:
Impact Studies ISBN: 9783642624575
The Alamo Breccia is a Late Devonian sedimentary layer as much as 135 m in thickness that is widespread over southern Nevada, USA. Direct evidence for an impact origin of the Alamo Breccia includes shocked quartz grains within the Breccia matrix and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0f42403db5ec83e4d9ce2d175aede2a1
https://doi.org/10.1007/978-3-642-55463-6_13
https://doi.org/10.1007/978-3-642-55463-6_13