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Record #139997:

Additional Rb-Sr and single-grain zircon datings of Caledonian granitoid rocks from Albert I Land, north-west Spitsbergen / Ju.A. Balašov, J.J. Peucat, A.M. Teben'kov, Y. Ohta, A.N. Larionov, A.N. Sirotkin.

Title: Additional Rb-Sr and single-grain zircon datings of Caledonian granitoid rocks from Albert I Land, north-west Spitsbergen / Ju.A. Balašov, J.J. Peucat, A.M. Teben'kov, Y. Ohta, A.N. Larionov, A.N. Sirotkin.
Author(s): Balašov, Ju. A.
Peucat, J. J.
Teben'kov, A. M.
Ohta, Y.
Larionov, A. N.
Sirotkin, A. N.
Date: 1996.
In: Polar Research. (1996.), Vol. 15(2) (1996)
Abstract: Previous K-Ar and Rb-Sr datings of metamorphic and granitic rocks from north-western basement region of Spitsbergen show main cooling time of rocks, except for Rb-Sr isochron age of Hornemantoppen granitoids and grey granites. Dioritic dyke was also dated by latter method. Bulk rock chemistry shows that most of both granitic rocks are of S-type and probably post- orogenic, incorporating crustal materials. Preliminary results from multi- grain zircon evaporation method imply Palaeo- and Mesoproterozoic protoliths for metamorphic rocks of this area.
Notes:

Polar Research. Vol. 15(2) :153-165 (1996).

Keywords: 54.027 -- Isotope analysis.
551.1/.4 -- Geology.
551.251 -- Metamorphism.
552.3 -- Igneous rocks.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 139997

MARCXML

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008 220929s1996####xx#ab#|##|###|0||#0|eng#d
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245 00 ‡aAdditional Rb-Sr and single-grain zircon datings of Caledonian granitoid rocks from Albert I Land, north-west Spitsbergen /‡cJu.A. Balašov, J.J. Peucat, A.M. Teben'kov, Y. Ohta, A.N. Larionov, A.N. Sirotkin.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1996.
300 ## ‡ap. 153-165 :‡bdiags., tables, map.
500 ## ‡aPolar Research. Vol. 15(2) :153-165 (1996).
520 3# ‡aPrevious K-Ar and Rb-Sr datings of metamorphic and granitic rocks from north-western basement region of Spitsbergen show main cooling time of rocks, except for Rb-Sr isochron age of Hornemantoppen granitoids and grey granites. Dioritic dyke was also dated by latter method. Bulk rock chemistry shows that most of both granitic rocks are of S-type and probably post- orogenic, incorporating crustal materials. Preliminary results from multi- grain zircon evaporation method imply Palaeo- and Mesoproterozoic protoliths for metamorphic rocks of this area.
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.251 -- Metamorphism.‡2udc
650 07 ‡a552.3 -- Igneous 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# ‡aBalašov, Ju. A.
700 1# ‡aPeucat, J. J.
700 1# ‡aTeben'kov, A. M.
700 1# ‡aOhta, Y.
700 1# ‡aLarionov, A. N.
700 1# ‡aSirotkin, A. N.
773 0# ‡7nnas ‡tPolar Research. ‡gVol. 15(2) (1996) ‡wSPRI-64246
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929