skip to primary navigation skip to content
 

 

You are not currently logged in

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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #135557:

Northern continuation of Caledonian high-pressure metamorphic rocks in central-western Spitsbergen / Y. Ohta, A.A. Krasil'ščikov, C. Lepvrier, A.M. Teben'kov.

Title: Northern continuation of Caledonian high-pressure metamorphic rocks in central-western Spitsbergen / Y. Ohta, A.A. Krasil'ščikov, C. Lepvrier, A.M. Teben'kov.
Author(s): Ohta, Y.
Krasil'ščikov, A. A.
Lepvrier, C.
Teben'kov, A. M.
Date: 1995.
In: Polar Research. (1995.), Vol. 14(3) (1995)
Abstract: Caledonian low-temperature, high-pressure metamorphic rocks, first recognised at Motalafjella, include characteristic brown dolostone and serpentinite. Similar rocks are scattered along sand flats and along local faults. Rocks contain high contents of MgO in carbonates and Cr₂O₃ in oxides. They seem to extend up to 50 km NNW from Motalafjella.
Notes:

Polar Research. Vol. 14(3) :303-315 (1995).

Keywords: 54 -- Chemistry.
551.1/.4 -- Geology.
552 -- Petrology.
552.4 -- Metamorphic rocks.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 135557

MARCXML

LDR 01313naa#a2200000#a#4500
001 SPRI-135557
005 20240419101854.0
007 ta
008 240419s1995####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-135557
040 ## ‡aUkCU-P‡beng‡eaacr
245 00 ‡aNorthern continuation of Caledonian high-pressure metamorphic rocks in central-western Spitsbergen /‡cY. Ohta, A.A. Krasil'ščikov, C. Lepvrier, A.M. Teben'kov.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1995.
300 ## ‡ap. 303-315 :‡bdiags., tables, maps.
500 ## ‡aPolar Research. Vol. 14(3) :303-315 (1995).
520 3# ‡aCaledonian low-temperature, high-pressure metamorphic rocks, first recognised at Motalafjella, include characteristic brown dolostone and serpentinite. Similar rocks are scattered along sand flats and along local faults. Rocks contain high contents of MgO in carbonates and Cr₂O₃ in oxides. They seem to extend up to 50 km NNW from Motalafjella.
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a552 -- Petrology.‡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(*32) -- Svalbard.‡2udc
700 1# ‡aOhta, Y.
700 1# ‡aKrasil'ščikov, A. A.
700 1# ‡aLepvrier, C.
700 1# ‡aTeben'kov, A. M.
773 0# ‡7nnas ‡tPolar Research. ‡gVol. 14(3) (1995) ‡wSPRI-64246
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240419