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Record #126247:
Salt diapirs, pore-water traps and permafrost as key controls for glaciotectonism in the Kiel area, northwestern Germany / Jan A. Piotrowski.
Title: | Salt diapirs, pore-water traps and permafrost as key controls for glaciotectonism in the Kiel area, northwestern Germany / Jan A. Piotrowski. |
Author(s): | Piotrowski, Jan A. |
Date: | 1993. |
Publisher: | Regina, Saskatchewan: University of Regina, Canadian Plains Research Center |
In: | Glaciotectonics and mapping glacial deposits. Proceedings of the INQUA Commission on Formation and Properties of Glacial Deposits. (1993.), |
Abstract: | Among mechanisms responsible for glaciotectonic deformation in this area, presence of heavily diapirized Permian salt structures in substratum, discontinuous confined aquifers of Weichselian age (pore-water traps), and permafrost wedge in front of Weichselian ice sheet seem to have been important. |
Notes: | In: Glaciotectonics and mapping glacial deposits. Proceedings of the INQUA Commission on Formation and Properties of Glacial Deposits / James S. Aber, ed. |
Keywords: | 551.33 -- Glacial geology. 551.333 -- Glacial deformation and glaciotectonic structures. E7 -- Glaciology: glacial geology and ice ages. (430) -- Germany. |
Location(s): | SCO: SPRI-SHF: 551.33 [1993] |
SPRI record no.: | 126247 |
LDR 01652naa#a2200000#a#4500 001 SPRI-126247 005 20230928121358.0 007 ta 008 230928s1993####sncabf#|#####|0||#0#eng#d 035 ## ‡aSPRI-126247 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aPiotrowski, Jan A. 245 10 ‡aSalt diapirs, pore-water traps and permafrost as key controls for glaciotectonism in the Kiel area, northwestern Germany /‡cJan A. Piotrowski. 260 ## ‡aRegina, Saskatchewan :‡bUniversity of Regina, Canadian Plains Research Center,‡c1993. 300 ## ‡ap. 86-98 :‡bdiags., maps, plates (between p.214 and 215) 490 0# ‡aCanadian Plains Proceedings ;‡v25 500 ## ‡aIn: Glaciotectonics and mapping glacial deposits. Proceedings of the INQUA Commission on Formation and Properties of Glacial Deposits / James S. Aber, ed. 520 3# ‡aAmong mechanisms responsible for glaciotectonic deformation in this area, presence of heavily diapirized Permian salt structures in substratum, discontinuous confined aquifers of Weichselian age (pore-water traps), and permafrost wedge in front of Weichselian ice sheet seem to have been important. 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.333 -- Glacial deformation and glaciotectonic structures.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(430) -- Germany.‡2udc 773 0# ‡7nnam ‡aJames S. Aber, ed. ‡tGlaciotectonics and mapping glacial deposits. Proceedings of the INQUA Commission on Formation and Properties of Glacial Deposits. ‡dRegina, Saskatchewan : University of Regina, Canadian Plains Research Center, 1993. ‡wSPRI-126240 852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h551.33 [1993]‡9Create 1 item record‡0Migrate 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230928