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Record #135563:
- #135563
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MARC recordGeology of an area astride the Billefjorden Fault Zone, northern Dickson Land, Spitsbergen, Svalbard / D.L. Lamar, D.N. Douglass.
| Title: | Geology of an area astride the Billefjorden Fault Zone, northern Dickson Land, Spitsbergen, Svalbard / D.L. Lamar, D.N. Douglass. |
| Author(s): | Lamar, D. L. Douglass, D. N. |
| Date: | 1995. |
| In: | Norsk Polarinstitutt. Skrifter. (1995.), Vol. 197 (1995) |
| Abstract: | Basement rocks consist of Precambrian Hecla Hoek schist, gneiss and amphibolite within fault-bounded block. Devonian Old Red Sandstone rocks are exposed in and west of fault zone. Balliolbreen, principal strand of fault zone, has reverse separation. Before being overlain by Carboniferous rocks, fault dipped eastwards. Folds are tight and overturned near fault. Moderate dip of individual strands of fault zone and fold pattern suggest EW compression and mainly reverse slip. |
| Notes: | Norsk Polarinstitutt. Skrifter. Vol. 197 :1-43 (1995). |
| Keywords: | 551.1/.4 -- Geology. 551.7 -- Stratigraphy. 551.71/.72 -- Precambrian. 551.734 -- Devonian. 551.735 -- Carboniferous. B -- Geology and soil sciences. (*3) -- Arctic regions. (*32) -- Svalbard. |
| SPRI record no.: | 135563 |
LDR 01449naa#a2200000#a#4500 001 SPRI-135563 005 20231003193714.0 007 ta 008 231003s1995####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-135563 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aLamar, D. L. 245 10 ‡aGeology of an area astride the Billefjorden Fault Zone, northern Dickson Land, Spitsbergen, Svalbard /‡cD.L. Lamar, D.N. Douglass. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1995. 300 ## ‡ap. 1-43 :‡bill., diags., maps (one in pocket) 500 ## ‡aNorsk Polarinstitutt. Skrifter. Vol. 197 :1-43 (1995). 520 3# ‡aBasement rocks consist of Precambrian Hecla Hoek schist, gneiss and amphibolite within fault-bounded block. Devonian Old Red Sandstone rocks are exposed in and west of fault zone. Balliolbreen, principal strand of fault zone, has reverse separation. Before being overlain by Carboniferous rocks, fault dipped eastwards. Folds are tight and overturned near fault. Moderate dip of individual strands of fault zone and fold pattern suggest EW compression and mainly reverse slip. 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a551.7 -- Stratigraphy.‡2udc 650 07 ‡a551.71/.72 -- Precambrian.‡2udc 650 07 ‡a551.734 -- Devonian.‡2udc 650 07 ‡a551.735 -- Carboniferous.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*32) -- Svalbard.‡2udc 700 1# ‡aDouglass, D. N. 773 0# ‡7nnas ‡tNorsk Polarinstitutt. Skrifter. ‡gVol. 197 (1995) ‡wSPRI-21042 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231003