Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Patti J. Burkett"'
Publikováno v:
Marine Geology. 150:39-50
Marine snow from upper and mid-water (i.e., pelagic) depths on the California margin is texturally and compositionally different from that traveling in the nepheloid layer. Transmission electron microscopy shows that pelagic marine snow consists prim
Autor:
Clyde A. Sapp, J. M. Dahl, Michael Long, Patti J. Burkett, Catherine M. Corrigan, Joseph Weir, Michael E. Zolensky
Publikováno v:
Meteoritics & Planetary Science. 32:509-515
— We have investigated the porosity of a large number of chondritic interplanetary dust particles (IDPs) and meteorites by three techniques: standard liquid/gas flow techniques, a new, noninvasive ultrasonic technique, and image processing of backs
Publikováno v:
Frontiers in Sedimentary Geology ISBN: 9781461287667
The consolidation of sediment is the main cause of porosity reduction with depth in the upper 1000 m of the marine sediment column and the process is mostly mechanical: the weight of the overlying sediment drives the rearrangement of the individual p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e937b249bf90544f5d7d724b13591865
https://doi.org/10.1007/978-1-4612-4428-8_7
https://doi.org/10.1007/978-1-4612-4428-8_7
Publikováno v:
Frontiers in Sedimentary Geology ISBN: 9781461287667
The objective of this study was to examine the microfabric of red clay sediments from the Central Pacific deep-sea basin using transmission electron microscopy by assessing the response of the fabric to thermal and mechanical influences resulting fro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f78c7cfb7d15a3784e732f066400394c
https://doi.org/10.1007/978-1-4612-4428-8_52
https://doi.org/10.1007/978-1-4612-4428-8_52
Publikováno v:
Frontiers in Sedimentary Geology ISBN: 9781461287667
The collection of high-quality sediment samples recovered from the sea floor is prerequisite to initiating laboratory investigations of sedimentological, microstructural, or geotechnical properties. These types of studies require virtually undisturbe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3d58aeb7cd1bdcec1134117096665044
https://doi.org/10.1007/978-1-4612-4428-8_35
https://doi.org/10.1007/978-1-4612-4428-8_35
Publikováno v:
Frontiers in Sedimentary Geology ISBN: 9781461287667
Convergent margins are one of three major geological boundaries in terms of relative plate motion. These margins are sites where large piles of sediment are being physically transferred from one tectonic plate to another, often forming the roots of e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c4de4ac922b46523aba70cb1f5f3fc0
https://doi.org/10.1007/978-1-4612-4428-8_22
https://doi.org/10.1007/978-1-4612-4428-8_22
Publikováno v:
Frontiers in Sedimentary Geology ISBN: 9781461287667
Shales generally are regarded as source rocks and seals. However, in the Illinois, Michigan, and Appalachian Basins, shales of Devonian age commonly are regarded as reservoir rocks. According to Broadhead et al. (1982), economic gas production from n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f2a87c14c713f2067205da9be473e79c
https://doi.org/10.1007/978-1-4612-4428-8_10
https://doi.org/10.1007/978-1-4612-4428-8_10
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