SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
Record #176586:
Lateral constraint rather than escape along a terrane boundary near Skelleftehamn / Christopher J. Talbot.
Title: | Lateral constraint rather than escape along a terrane boundary near Skelleftehamn / Christopher J. Talbot. |
Author(s): | Talbot, Christopher J. |
Date: | 2005. |
In: | GFF. (2005.), Vol. 127(2) (2005) |
Abstract: | Describes characteristics of two suites of greywackes cropping out to north and south of Skellefte River. Differences suggest that greywackes formed on different sides of Bothnian palaeo-ocean at different times. Deep reflection profiles across region indicate orogenic wedge defined by two suites of imbricate thrusts converging downwards to significant offset in Moho. Notes that mylonites of Skellefte terrane boundary juxtapose southern terrane of old gneisses deformed at great depth against northern terrane that never reached such depths. |
Notes: | GFF. Vol. 127(2) :99-114 (2005). |
Keywords: | 551.1/.4 -- Geology. 551.22 -- Volcanism, intrusions. 551.241 -- Plate tectonics. 551.72 -- Proterozoic. 552.514 -- Greywacke. B -- Geology and soil sciences. (*3) -- Arctic regions. (*57) -- Sweden. (*571) -- Norrland. |
SPRI record no.: | 176586 |
LDR 01480naa#a2200000#a#4500 001 SPRI-176586 005 20231204172050.0 007 ta 008 231204s2005####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-176586 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aTalbot, Christopher J. 245 10 ‡aLateral constraint rather than escape along a terrane boundary near Skelleftehamn /‡cChristopher J. Talbot. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2005. 300 ## ‡ap. 99-114 :‡bill., diags., maps. 500 ## ‡aGFF. Vol. 127(2) :99-114 (2005). 520 3# ‡aDescribes characteristics of two suites of greywackes cropping out to north and south of Skellefte River. Differences suggest that greywackes formed on different sides of Bothnian palaeo-ocean at different times. Deep reflection profiles across region indicate orogenic wedge defined by two suites of imbricate thrusts converging downwards to significant offset in Moho. Notes that mylonites of Skellefte terrane boundary juxtapose southern terrane of old gneisses deformed at great depth against northern terrane that never reached such depths. 650 07 ‡a551.1/.4 -- Geology.‡2udc 650 07 ‡a551.22 -- Volcanism, intrusions.‡2udc 650 07 ‡a551.241 -- Plate tectonics.‡2udc 650 07 ‡a551.72 -- Proterozoic.‡2udc 650 07 ‡a552.514 -- Greywacke.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*57) -- Sweden.‡2udc 651 #7 ‡a(*571) -- Norrland.‡2udc 773 0# ‡7nnas ‡tGFF. ‡gVol. 127(2) (2005) ‡wSPRI-128316 916 ## ‡aJW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231204 ‡bJW