Zobrazeno 1 - 10
of 160
pro vyhledávání: '"M.D. Max"'
Autor:
Zajonc, Dirk M., Crispin, M.D. Max, Bowden, Thomas A., Young, David C., Cheng, Tan-Yun, Hu, Jingdan, Costello, Catherine E., Rudd, Pauline M., Dwek, Raymond A., Miller, Marvin J., Brenner, Michael B., Moody, D. Branch, Wilson, Ian A. *
Publikováno v:
In Immunity 2005 22(2):209-219
Autor:
M.D. Max, A.H. Johnson
Publikováno v:
Petroleum Geoscience. 18:231-238
Many of the original muddy marine sediments that have compacted to become gas shale could have been in a depositional environment suitable for the formation of natural gas hydrate (NGH), which concentrates gas by a factor of 164 (at STP). Dispersed b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb48ff7b343c86c08ec6fbf98776fdee
https://doi.org/10.1144/1354-079311-035
https://doi.org/10.1144/1354-079311-035
Publikováno v:
Energy Procedia. 1:4961-4968
Carbon sequestration (CO2 disposal) may be only a temporary measure for bridging from the current situation in which carbon emissions to the atmosphere are unacceptably high and increasing, to a carbon-free economy, but it is a practical and immediat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29030243973444fdce56032b577b766c
https://doi.org/10.1016/j.egypro.2009.02.328
https://doi.org/10.1016/j.egypro.2009.02.328
Publikováno v:
Marine and Petroleum Geology. 17:929-936
Marine sediments on the continental slope of the NE South China Sea have appropriate thickness, methane-generating potential, and occur in a suitable pressure–temperature regime to host gas hydrate. Evidence for gas hydrate, the bottom simulating r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e392029f7ac56071ffe450b173845cc1
https://doi.org/10.1016/s0264-8172(00)00023-4
https://doi.org/10.1016/s0264-8172(00)00023-4
Publikováno v:
Marine and Petroleum Geology. 16:41-64
New aeromagnetics show a complex of magnetic patterns and source depths of the north and central Argentine continental and adjacent oceanic crust. The 40 km wide, positive magnetic G-anomaly reflects an end-rift associated volcanic edifice at the con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7574eba8f449f1c9618a34935e981afd
https://doi.org/10.1016/s0264-8172(98)00063-4
https://doi.org/10.1016/s0264-8172(98)00063-4
Autor:
M.D. Max
1. THE BEGINNINGS OF HYDRATE RESEARCH Until very recently, our understanding of hydrate in the natural environment and its impact on seafloor stability, its importance as a sequester of methane, and its potential as an important mechanism in the Eart
Autor:
Kauther, M.D. (Max)
Retrospektive Untersuchung von 25 operativ therapierten Patienten mit hochgradigem Morbus Scheuermann über durchschnittlich 46,7 Monate. Therapieindikationen sind progrediente Kyphosierung, Schmerzen und Leidensdruck. Die durchschnittliche maximale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______517::d12681aaefec678aa1bafff0134e4a6f
https://repositorium.uni-muenster.de/transfer/miami/085b8d76-52aa-47fa-93c4-36bf49651079
https://repositorium.uni-muenster.de/transfer/miami/085b8d76-52aa-47fa-93c4-36bf49651079
Publikováno v:
Journal of Petroleum Geology. 21
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c5082ad007b8785427a4dd8143602a9f
https://doi.org/10.1306/bf9ab7ab-0eb6-11d7-8643000102c1865d
https://doi.org/10.1306/bf9ab7ab-0eb6-11d7-8643000102c1865d
Autor:
Weinberg, M.D., Max H.
Publikováno v:
Confinia Neurologica; 1939, Vol. 2 Issue 1/2, p292-302, 11p
Autor:
M.D. Max, John A. Winchester
Publikováno v:
Precambrian Research. 45:191-201
Field evidence shows the Late Proterozoic Erris Group of NW Ireland to be a clastic succession deposited in an intracratonic basin and subsequently metamorphosed during the Caledonian event. The lower formations of the group tend to consist mainly of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fd85ac3f8ab94268f17d6054b04d0953
https://doi.org/10.1016/0301-9268(89)90039-9
https://doi.org/10.1016/0301-9268(89)90039-9