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Record #155431:
The Pasterze glacier, Austria: an analogue of an extensional allochthon / Paul Herbst, Franz Neubauer.
Title: | The Pasterze glacier, Austria: an analogue of an extensional allochthon / Paul Herbst, Franz Neubauer. |
Author(s): | Herbst, Paul. Neubauer, Franz. |
Date: | 2000. |
Publisher: | London: Geological Society |
In: | Deformation of glacial materials. (2000.), |
Abstract: | Uses structures of Pasterze glacier, Austria to represent natural model of extensional allochthon formed over orogenic wedge, and model for raft tectonics at passive continental margins. Structures at lower part of glacier form close to melting point of ice, with brittle structures near to surface. Defines three flow units. Finds glacial flow more rapid in middle to upper sectors of glacier than along lateral, lower margins. Distinguishes three structural domains in lower, ablation-controlled sector of glacier, found also in Neogene Alpine-Carpathian system, and recent models and examples of passive continental margins. |
Notes: | In: Deformation of glacial materials / Alex J. Maltman, Bryn Hubbard, Michael J. Hambrey, eds. |
Keywords: | 551.32 -- Glaciology. 551.324 -- Land ice. 551.324.22 -- Glaciers: Pasterze. 551.324.5 -- Land ice, flow. 551.33 -- Glacial geology. 519.673 -- Modelling. E5 -- Glaciology: land ice. (436) -- Austria. |
SPRI record no.: | 155431 |
LDR 01698naa#a2200000#a#4500 001 SPRI-155431 005 20240329135045.0 007 ta 008 240329s2000####enka###|#####|0||#0#eng#d 035 ## ‡aSPRI-155431 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aHerbst, Paul. 245 14 ‡aThe Pasterze glacier, Austria :‡ban analogue of an extensional allochthon /‡cPaul Herbst, Franz Neubauer. 260 ## ‡aLondon :‡bGeological Society,‡c2000. 300 ## ‡ap. 159-168 :‡bill., diags. 500 ## ‡aIn: Deformation of glacial materials / Alex J. Maltman, Bryn Hubbard, Michael J. Hambrey, eds. 520 3# ‡aUses structures of Pasterze glacier, Austria to represent natural model of extensional allochthon formed over orogenic wedge, and model for raft tectonics at passive continental margins. Structures at lower part of glacier form close to melting point of ice, with brittle structures near to surface. Defines three flow units. Finds glacial flow more rapid in middle to upper sectors of glacier than along lateral, lower margins. Distinguishes three structural domains in lower, ablation-controlled sector of glacier, found also in Neogene Alpine-Carpathian system, and recent models and examples of passive continental margins. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a551.324.22 -- Glaciers: Pasterze.‡2udc 650 07 ‡a551.324.5 -- Land ice, flow.‡2udc 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(436) -- Austria.‡2udc 700 1# ‡aNeubauer, Franz. 773 0# ‡7nnam ‡aAlex J. Maltman, Bryn Hubbard, Michael J. Hambrey, eds. ‡tDeformation of glacial materials. ‡dLondon : Geological Society, 2000. ‡wSPRI-154378 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240329