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Record #171205:
- #171205
Main publication details
MARC recordCarbon and oxygen isotopic survey of diagenetic carbonate deposits in the Agardhfjellet Formation (Upper Jurassic), Spitsbergen: preliminary results / Krzysztof P. Krajewski.
| Title: | Carbon and oxygen isotopic survey of diagenetic carbonate deposits in the Agardhfjellet Formation (Upper Jurassic), Spitsbergen: preliminary results / Krzysztof P. Krajewski. |
| Author(s): | Krajewski, Krzysztof P. |
| Date: | 2004. |
| In: | Polish Polar Research. (2004.), Vol. 25(1) (2004) |
| Abstract: | Concretions, cementation bodies and bands are common, dominated by dolomite/ankerite and siderite. They originated from displacement of host sediment in range from shallow sub-surface to deep burials. Isotope proportions suggest major stage of formation occurred under increased temperature. Carbon for precipitation was derived from dissolution of skeletal carbonate and decomposition of organic matter. |
| Notes: | Polish Polar Research. Vol. 25(1) :27-43 (2004). |
| Keywords: | 547 -- Chemistry, organic. 550.4 -- Geochemistry. 551.3.051 -- Sedimentation and stratification. 551.762 -- Jurassic. B -- Geology and soil sciences. (*3) -- Arctic regions. (*32) -- Svalbard. |
| SPRI record no.: | 171205 |
LDR 01406naa#a2200000#a#4500 001 SPRI-171205 005 20231207144754.0 007 ta 008 231207s2004####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-171205 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aKrajewski, Krzysztof P. 245 10 ‡aCarbon and oxygen isotopic survey of diagenetic carbonate deposits in the Agardhfjellet Formation (Upper Jurassic), Spitsbergen :‡bpreliminary results /‡cKrzysztof P. Krajewski. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2004. 300 ## ‡ap. 27-43 :‡bill., diags., table, map. 500 ## ‡aPolish Polar Research. Vol. 25(1) :27-43 (2004). 520 3# ‡aConcretions, cementation bodies and bands are common, dominated by dolomite/ankerite and siderite. They originated from displacement of host sediment in range from shallow sub-surface to deep burials. Isotope proportions suggest major stage of formation occurred under increased temperature. Carbon for precipitation was derived from dissolution of skeletal carbonate and decomposition of organic matter. 650 07 ‡a547 -- Chemistry, organic.‡2udc 650 07 ‡a550.4 -- Geochemistry.‡2udc 650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc 650 07 ‡a551.762 -- Jurassic.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*32) -- Svalbard.‡2udc 773 0# ‡7nnas ‡tPolish Polar Research. ‡gVol. 25(1) (2004) ‡wSPRI-60789 916 ## ‡a2005/10/18 -- JP 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231207 ‡bJP