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Record #110658:
- #110658
Main publication details
MARC recordReservoir evaluation of Upper Permian buildups in the Jameson Land basin, East Greenland / Lars Stemmerik.
| Title: | Reservoir evaluation of Upper Permian buildups in the Jameson Land basin, East Greenland / Lars Stemmerik. |
| Author(s): | Stemmerik, Lars. |
| Date: | 1991. |
| In: | Grønlands Geologiske Undersøgelse. Rapport. (1991.), Vol. 149 (1991) |
| Abstract: | Reservoir potential is mainly confined to buildup cores and proximal flank deposits. Porosity prior to hydrocarbon migration is estimated to average 10% in buildups and 5-6% in proximal flank deposits. Pores became filled by hydrocarbons probably in Late Cretaceous; reservoirs became flushed by hot, hydrothermal fluids c. 20 Ma ago and pores are now filled by iron-rich calcite, baryte and fluorite. Flushing of reservoir may be related to Tertiary uplift of Wegener Halvø, and it is most probably local event not affecting basin as whole. |
| Notes: | Grønlands Geologiske Undersøgelse. Rapport. Vol. 149 :1-24 (1991). |
| Keywords: | 550.8 -- Geology and geophysics, applied. 551.7 -- Stratigraphy. 551.736 -- Permian. 553 -- Economic geology. 553.9 -- Hydrocarbon minerals. B -- Geology and soil sciences. (*38) -- Greenland. (*381.4) -- Kong Christian den Xs Land. |
| SPRI record no.: | 110658 |
LDR 01535naa#a2200000#a#4500 001 SPRI-110658 005 20230321214626.0 007 ta 008 230321s1991####xx#abf|##|###|0||#0|eng#d 035 ## ‡aSPRI-110658 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aStemmerik, Lars. 245 10 ‡aReservoir evaluation of Upper Permian buildups in the Jameson Land basin, East Greenland /‡cLars Stemmerik. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 1-24 :‡bill., diags., tables, maps, plates. 500 ## ‡aGrønlands Geologiske Undersøgelse. Rapport. Vol. 149 :1-24 (1991). 520 3# ‡aReservoir potential is mainly confined to buildup cores and proximal flank deposits. Porosity prior to hydrocarbon migration is estimated to average 10% in buildups and 5-6% in proximal flank deposits. Pores became filled by hydrocarbons probably in Late Cretaceous; reservoirs became flushed by hot, hydrothermal fluids c. 20 Ma ago and pores are now filled by iron-rich calcite, baryte and fluorite. Flushing of reservoir may be related to Tertiary uplift of Wegener Halvø, and it is most probably local event not affecting basin as whole. 650 07 ‡a550.8 -- Geology and geophysics, applied.‡2udc 650 07 ‡a551.7 -- Stratigraphy.‡2udc 650 07 ‡a551.736 -- Permian.‡2udc 650 07 ‡a553 -- Economic geology.‡2udc 650 07 ‡a553.9 -- Hydrocarbon minerals.‡2udc 650 07 ‡aB -- Geology and soil sciences.‡2local 651 #7 ‡a(*38) -- Greenland.‡2udc 651 #7 ‡a(*381.4) -- Kong Christian den Xs Land.‡2udc 773 0# ‡7nnas ‡tGrønlands Geologiske Undersøgelse. Rapport. ‡gVol. 149 (1991) ‡wSPRI-39401 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230321