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Record #201636:

Formation history and physical properties of sediments from the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope / Sheng Dai, Changho Lee, J. Carlos Santamarina.

Title: Formation history and physical properties of sediments from the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope / Sheng Dai, Changho Lee, J. Carlos Santamarina.
Author(s): Dai, Sheng.
Lee, Changho.
Santamarina, J. Carlos.
Date: 2011.
Publisher: [Amsterdam]: Elsevier
Abstract: Reports findings of synthesis of available geological information and surface temperature evolution in Alaska North Slope region. Biogenic and deeper thermogenic gases migrated through fault networks and preferentially invaded coarse-grained layers with high hydraulic conductivity and low gas entry pressures. Hydrate started forming before beginning of permafrost. Eventually permafrost deepened and any remaining free water froze, so that ice and hydrate may coexist at some elevations.
Notes:

Offprint: Marine and Petroleum Geology. Vol. 28.

Keywords: 550.834 -- Seismic survey methods.
551.1/.4 -- Geology.
551.345 -- Permafrost. Cryopedology.
552.3 -- Igneous rocks.
553 -- Economic geology.
553.98 -- Hydrocarbon deposits.
553.981 -- Natural gas.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*49) -- Alaska.
(*494) -- Alaska, northwestern.
Location(s): SCO: SPRI-PAM: (*49) : 553.98
SPRI record no.: 201636

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035 ## ‡aSPRI-201636
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aDai, Sheng.
245 10 ‡aFormation history and physical properties of sediments from the Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope /‡cSheng Dai, Changho Lee, J. Carlos Santamarina.
260 ## ‡a[Amsterdam] :‡bElsevier,‡c2011.
300 ## ‡ap. 427-438 :‡bill. (some col.), diags., tables ;‡c30 cm.
490 0# ‡aMarine and Petroleum Geology
500 ## ‡aOffprint: Marine and Petroleum Geology. Vol. 28.
520 3# ‡aReports findings of synthesis of available geological information and surface temperature evolution in Alaska North Slope region. Biogenic and deeper thermogenic gases migrated through fault networks and preferentially invaded coarse-grained layers with high hydraulic conductivity and low gas entry pressures. Hydrate started forming before beginning of permafrost. Eventually permafrost deepened and any remaining free water froze, so that ice and hydrate may coexist at some elevations.
530 ## ‡aAlso issued online ‡uurn:doi:10.1016/j.marpetgeo.2010.03.005‡uhttps://dx.doi.org/10.1016/j.marpetgeo.2010.03.005
650 07 ‡a550.834 -- Seismic survey methods.‡2udc
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.345 -- Permafrost. Cryopedology.‡2udc
650 07 ‡a552.3 -- Igneous rocks.‡2udc
650 07 ‡a553 -- Economic geology.‡2udc
650 07 ‡a553.98 -- Hydrocarbon deposits.‡2udc
650 07 ‡a553.981 -- Natural gas.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*49) -- Alaska.‡2udc
651 #7 ‡a(*494) -- Alaska, northwestern.‡2udc
700 1# ‡aLee, Changho.
700 1# ‡aSantamarina, J. Carlos.
852 7# ‡2camdept‡bSCO‡cSPRI-PAM‡h(*49) : 553.98‡9Create 1 item record‡0Migrate
916 ## ‡a147075 -- 2012/12/03 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329 ‡bJW