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Record #18111:
- #18111
Main publication details
MARC recordZur Tektonik der Ostküste von Grönland / Hans Cloos.
| Title: | Zur Tektonik der Ostküste von Grönland / Hans Cloos. |
| Translated title: | On the tectonics of the east coast of Greenland. |
| Author(s): | Cloos, Hans. |
| Date: | 1939. |
| Language: | German. |
| Abstract: | Author comments on papers of Bütler, Vischer, Stauber and Bierther. Tectonics is explained by area's being continental rim. Two questions are raised: has stretching been in control - was movement horizontal or vertical? and how does newly investigated stretch of coast relate to its southerly continuation? First answer is that movement is linked to uplift in centre spilling horizontal material into sinking area around it. Second is that metamorphic base is overlaid by massive basalt sheet. Rim is hinge of continental uplift with oceanic sinking of many kilometres. |
| Notes: | Offprint: Naturforschenden Gesellschaft Schaffhausen (Schweiz) Mitteilungen 16. Vol. 14 :179-181. |
| Keywords: | 551.1/.4 -- Geology. 551.24 -- Geotectonics. 552.323.5 -- Basalt. 552.4 -- Metamorphic rocks. B -- Geology and soil sciences. (*3) -- Arctic regions. (*38) -- Greenland. |
| Location(s): | SCO: SPRI-SHF: (*38) : 551.1/.4 |
| SPRI record no.: | 18111 |
LDR 01538nam#a2200000#a#4500 001 SPRI-18111 005 20230607231311.0 007 ta 008 230607s1939####xx####|##|###|0||#0|ger#d 035 ## ‡aSPRI-18111 040 ## ‡aUkCU-P‡beng‡eaacr 041 0# ‡ager 100 1# ‡aCloos, Hans. 242 10 ‡aOn the tectonics of the east coast of Greenland.‡yeng 245 10 ‡aZur Tektonik der Ostküste von Grönland /‡cHans Cloos. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1939. 300 ## ‡ap. 179-181. 500 ## ‡aOffprint: Naturforschenden Gesellschaft Schaffhausen (Schweiz) Mitteilungen 16. Vol. 14 :179-181. 520 3# ‡aAuthor comments on papers of Bütler, Vischer, Stauber and Bierther. Tectonics is explained by area's being continental rim. Two questions are raised: has stretching been in control - was movement horizontal or vertical? and how does newly investigated stretch of coast relate to its southerly continuation? First answer is that movement is linked to uplift in centre spilling horizontal material into sinking area around it. Second is that metamorphic base is overlaid by massive basalt sheet. Rim is hinge of continental uplift with oceanic sinking of many kilometres. 546 ## ‡aIn German. 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a551.24 -- Geotectonics.‡2udc 650 07 ‡a552.323.5 -- Basalt.‡2udc 650 07 ‡a552.4 -- Metamorphic rocks.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*38) -- Greenland.‡2udc 852 7# ‡2camdept‡bSCO‡cSPRI-SHF‡h(*38) : 551.1/.4‡9Create 1 item record‡0Migrate 916 ## ‡a117900 -- 1998/07/02 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230607