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Record #96633:
- #96633
Main publication details
MARC recordElectrical resistivity sounding related to ice-crystal size: a technique for probing the Holocene-Wisconsin boundary (abstract) / Sion Shabtaie, Charles R. Bentley.
| Title: | Electrical resistivity sounding related to ice-crystal size: a technique for probing the Holocene-Wisconsin boundary (abstract) / Sion Shabtaie, Charles R. Bentley. |
| Author(s): | Shabtaie, Sion. Bentley, Charles R. |
| Date: | 1989. |
| Publisher: | Cambridge: International Glaciological Society |
| In: | Annals of Glaciology. (1989.), Vol. 12 (1989) |
| Abstract: | Measurements and model studies at several locations in Antarctica have resulted in discovery of rather sharp change in resistivity at depth identified with Holocene/Wisconsin transition at two locations. This change may be attributed primarily to changes in crystal size. At one location on Ice Stream B, where ice is 1060 m thick, best model using this relationship shows Holocene-Wisconsin boundary at 750 m depth. |
| Notes: | Annals of Glaciology. Vol. 12 :207-208 (1989). |
| Keywords: | 551.324.8 -- Land ice, structure and surface features. 551.32 -- Glaciology. 551.324 -- Land ice. 537 -- Electricity. 548.54 -- Ice crystals, habit and appearance. E5 -- Glaciology: land ice. (*7) -- Antarctic regions. |
| SPRI record no.: | 96633 |
LDR 01422naa#a2200000#a#4500 001 SPRI-96633 005 20231202175936.0 007 ta 008 231202s1989####enk###|##|###|0||#0|eng#d 035 ## ‡aSPRI-96633 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aShabtaie, Sion. 245 10 ‡aElectrical resistivity sounding related to ice-crystal size :‡ba technique for probing the Holocene-Wisconsin boundary (abstract) /‡cSion Shabtaie, Charles R. Bentley. 260 ## ‡aCambridge :‡bInternational Glaciological Society,‡c1989. 300 ## ‡ap. 207-208. 500 ## ‡aAnnals of Glaciology. Vol. 12 :207-208 (1989). 520 3# ‡aMeasurements and model studies at several locations in Antarctica have resulted in discovery of rather sharp change in resistivity at depth identified with Holocene/Wisconsin transition at two locations. This change may be attributed primarily to changes in crystal size. At one location on Ice Stream B, where ice is 1060 m thick, best model using this relationship shows Holocene-Wisconsin boundary at 750 m depth. 650 07 ‡a551.324.8 -- Land ice, structure and surface features.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.324 -- Land ice.‡2udc 650 07 ‡a537 -- Electricity.‡2udc 650 07 ‡a548.54 -- Ice crystals, habit and appearance.‡2udc 650 07 ‡aE5 -- Glaciology: land ice.‡2local 651 #7 ‡a(*7) -- Antarctic regions.‡2udc 700 1# ‡aBentley, Charles R. 773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 12 (1989) ‡wSPRI-60773 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231202