Zobrazeno 1 - 10 of 16 pro vyhledávání: '"B. C. Schreiber"'
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Akademický článek
Thenardite after mirabilite deposits as a cool climate indicator in the geological record: lower Miocene of central Spain
Autor: M. J. Herrero, J. I. Escavy, B. C. Schreiber
Publikováno v: Climate of the Past, Vol 11, Iss 1, Pp 1-13 (2015)
Salt deposits are commonly used as indicators of different paleoclimates and sedimentary environments, as well as being geological resources of great economic interest. Ordinarily, the presence of salt deposits is related to warm and arid environment
Externí odkaz: https://doaj.org/article/07db6348b97c48f6a12b72ce6cc1619f
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2
Physical abrasion of mafic minerals and basalt grains: Application to martian aeolian deposits
Autor: Carin Cornwall, Joshua L. Bandfield, B. C. Schreiber, David R. Montgomery, Timothy N. Titus
Publikováno v: Icarus. 256:13-21
Sediment maturity, or the mineralogical and physical characterization of sedimentary deposits, has been used to identify sediment sources, transport medium and distance, weathering processes, and paleoenvironments on Earth. Mature terrestrial sands a
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::653a39528ce23992f907b2ced8c519b9
https://doi.org/10.1016/j.icarus.2015.04.020
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3
Dense shelf water cascading and Messinian Canyons: A new scenario for the Mediterranean salinity crisis
Autor: Rocco Gennari, Andrea Bergamasco, Stefano Lugli, Marco Roveri, Vinicio Manzi, B. C. Schreiber, Francesco Marcello Falcieri
Publikováno v: American journal of science (1880) 314 (2014): 751–784. doi:10.2475/05.2014.03
info:cnr-pdr/source/autori:Roveri, M.; Manzi, V.; Bergamasco, A.; Falcieri, F. M.; Gennari, R.; Lugli, S.; Schreiber, B. C./titolo:DENSE SHELF WATER CASCADING AND MESSINIAN CANYONS: A NEW SCENARIO FOR THE MEDITERRANEAN SALINITY CRISIS/doi:10.2475%2F05.2014.03/rivista:American journal of science (1880)/anno:2014/pagina_da:751/pagina_a:784/intervallo_pagine:751–784/volume:314
The salt giant beneath the deep Mediterranean seafloor is the impressive record of the “Messinian salinity crisis,” a dramatic event that occurred about 6 Ma ago following the reduction of the connections with the Atlantic Ocean. According to the
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3abf0d4bdebfc9836adf0e3d50d8a207
https://doi.org/10.2475/05.2014.03
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4
Dredged rocks from Hatton Bank, Rockall Plateau
Autor: D. Habib, B. C. Schreiber, Anthony Watts
Three dredge hauls were obtained in I973 by R/V Vema from the northern slopes of Hatton Bank. The most common rock types in each haul are arkosic and subarkosic arenite. The arkosic arenite is associated with other sedimentary rocks which include fos
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ef25bc6f06ad8b17a38c3eb2553ff379
https://doi.org/10.1144/gsjgs.131.6.0639
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5
The Messinian 'Calcare di Base' (Sicily, Italy) revisited
Autor: Rocco Gennari, Stefano Lugli, B. C. Schreiber, Vinicio Manzi, Marco Roveri
Publikováno v: Geological Society of America Bulletin. 123:347-370
Three different types of carbonate deposits are included within the "Calcare di Base," commonly envisaged to record the Messinian salinity crisis onset: type 1 consists of sulfur-bearing limestones, representing the biogenic product of bacterial sulf
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::dd78676b296d1f82369e6de4473de6e0
https://doi.org/10.1130/b30262.1
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6
Salt tectonics and collapse of Hebes Chasma, Valles Marineris, Mars
Autor: Alan R. Gillespie, Tim P. Dooley, Martin P. A. Jackson, David R. Montgomery, John B. Adams, B. C. Schreiber, Jean-Philippe Combe
Publikováno v: Geology. 37:691-694
A photogeologic and physical modeling study indicates that Hebes Chasma, Mars, formed by collapse of the megaregolith. Local heating facilitated drainage of ~10 5 km 3 of brines and entrained particulates through fractures in the chasma floor and int
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::bc8b1df87565774d896a703b5392c606
https://doi.org/10.1130/g30024a.1
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8
Messinian Salinity Crisis - Facts, Theories, Open Problems and their Implications for Mediterranean Exploration
Autor: Marco Roveri, Nicola Minelli, Vinicio Manzi, Rocco Gennari, Stefano Lugli, B. C. Schreiber, Matteo Reghizzi
Publikováno v: Proceedings.
A large consensus has been reached on a three-stage evolutionary model of the Messinian salinity crisis (MSC), each of them characterized by a peculiar association of evaporitic deposits, which record changes in the Mediterranean basin hydrology. How
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::be797a5ee40578607bfd3f7f8eba54b0
https://doi.org/10.3997/2214-4609.201413560
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9
Thenardite after mirabilite deposits as a cool climate indicator in the geological record: lower Miocene of central Spain
Autor: B. C. Schreiber, J.I. Escavy, M. J. Herrero
Publikováno v: E-Prints Complutense. Archivo Institucional de la UCM
instname
Climate of the Past, Vol 11, Iss 1, Pp 1-13 (2015)
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Evaporites are commonly used as indicators of different paleoclimates and sedimentary environments, as well as being geological resources of great economic interest. Ordinarily the presence of evaporites is related to warm and arid environmental cond
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::790be1f23cf1283f4ae4d43154d6cc7e
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