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Record #125609:
Interpretations of radar-detected internal layer folding in west Antarctic ice streams / Robert W. Jacobel, Anthony M. Gades, David L. Gottschling, Steven M. Hodge, David L. Wright.
Title: | Interpretations of radar-detected internal layer folding in west Antarctic ice streams / Robert W. Jacobel, Anthony M. Gades, David L. Gottschling, Steven M. Hodge, David L. Wright. |
Author(s): | Jacobel, Robert W. Gades, Anthony M. Gottschling, David L. Hodge, Steven M. Wright, David L. |
Date: | 1993. |
In: | Journal of Glaciology. (1993.), Vol. 39(133) (1993) |
Abstract: | Images depicting folding of internal layers can aid in interpretation of ice-stream dynamics. These structures are not related to bedrock topography and show tilting of axial fold planes in flow direction. Data show that they originate upstream of region of streaming flow and are advected into ice streams. Mechanism for producing folds is hypothesized to be changes in basal boundary conditions as ice makes transition from inland ice to ice-stream flow. Migration of this transition zone headward can then cause folds in internal layering to be propagated down ice stream. |
Notes: | Journal of Glaciology. Vol. 39(133) :528-537 (1993). |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.29 -- Land ice, miscellaneous forms. 551.324.81 -- Glacier bands, lamination, layering and foliation. 53.087.23 -- Remote sensing. 621.396.96 -- Radar. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. (*7.7) -- West Antarctica. |
SPRI record no.: | 125609 |
LDR 01778naa#a2200000#a#4500 001 SPRI-125609 005 20240419042058.0 007 ta 008 240419s1993####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-125609 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aInterpretations of radar-detected internal layer folding in west Antarctic ice streams /‡cRobert W. Jacobel, Anthony M. Gades, David L. Gottschling, Steven M. Hodge, David L. Wright. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 528-537 :‡bill., diags., maps. 500 ## ‡aJournal of Glaciology. Vol. 39(133) :528-537 (1993). 520 3# ‡aImages depicting folding of internal layers can aid in interpretation of ice-stream dynamics. These structures are not related to bedrock topography and show tilting of axial fold planes in flow direction. Data show that they originate upstream of region of streaming flow and are advected into ice streams. Mechanism for producing folds is hypothesized to be changes in basal boundary conditions as ice makes transition from inland ice to ice-stream flow. Migration of this transition zone headward can then cause folds in internal layering to be propagated down ice stream. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.29 -- Land ice, miscellaneous forms.‡2udc 650 07 ‡a551.324.81 -- Glacier bands, lamination, layering and foliation.‡2udc 650 07 ‡a53.087.23 -- Remote sensing.‡2udc 650 07 ‡a621.396.96 -- Radar.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 651 #7 ‡a(*7.7) -- West Antarctica.‡2udc 700 1# ‡aJacobel, Robert W. 700 1# ‡aGades, Anthony M. 700 1# ‡aGottschling, David L. 700 1# ‡aHodge, Steven M. 700 1# ‡aWright, David L. 773 0# ‡7nnas ‡tJournal of Glaciology. ‡gVol. 39(133) (1993) ‡wSPRI-20534 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240419