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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1118.txt | all","id":"par0015"},"#name":"para","_":"The Farsund intrusion was emplaced close to a shear zone and the opx-in isograd."}],"$":{"id":"lsti0015"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0020"},"#name":"para","_":"Limited differentiation occurred within each facies in the upper... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_6.txt | ±2 Åhäll & Connelly, 1998
Stigfjorden granite Zrn U-Pb 1503 ±3 Åhäll & Connelly, 1998
Norstrand-Sørmarka granodiorite, TA121 Zrn U-Pb 1517 ±12 Andersen et al., 2004
Hisingen suite, Hällungen granodiorite Zrn U-Pb 1530 ±6 Åhäll & Connelly, 2008
Hisingen suite, Grann granite Zrn U- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_26.txt | & Ask, 2006
PZ Vaggeryd syenite, 320 Zrn U-Pb 1219 ±3 Söderlund & Ask, 2006
PZ Vaggeryd syenite, 19.5 Zrn U-Pb 1220 ±3 Söderlund & Ask, 2006
PZ Anorthosite gabbro in Vaggeryd syenite, 209.2 Zrn U-Pb 1220 ±3 Söderlund & Ask, 2006
PZ Pegmatite dyke in Vaggeryd syenite, 19. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_105.txt | und, 1997
South Granitoid, Hesta suite, Lake Åsunden, 2 Am Low. intercept 8 956 ±4 Connelly et al., 1996
South Interboudin granite pegmatite, EAH0207 Am 207Pb/206Pb 8 961 ±26 Austin Hegardt et al., 2005
South Aplitic dyke, Vråna, 3 Am Up. intercept 7 1457 ±7 Connelly et al., 1996
South Migmatitic orthogneiss, Vistberge... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_30.txt | 48 0.0031 1.88 0.08 0.182 0.002 0.30 1064 83 1076 13 101.1
14 0.0750 0.0028 1.82 0.07 0.176 0.003 0.36 1067 75 1047 14 98.1
4 0.0933 0.0016 3.24 0.08 0.251 0.004 0.71 1494 33 1446 23 96.8
(1) Ratio corrected for common Pb, using mean terrestrial isotopic composition at 1500 Ma (Stacey | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_45.txt | models the Idefjorden terrane is part
of the margin of Fennoscandia and the Bamble-Kongsberg sector is regarded as the original collision zone
between Telemarkia and the Idefjorden terrane. The
main reasons for this interpretation are as follows. (1)
The Bamble-Kongsberg sector was affected by the earliest
recorded Sv... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_585.txt | new field, petrological and geochronological data from the SMB, as well as from para- and orthogneiss xenoliths within and forming the host rocks of the SMB. These data provide new constraints on the timing and character of magmatic and metamorphic events in the SW part of the Sveconorwegian orogen. We focus on primar... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_107.txt | 206Pb 1 1676 c. Söderlund et al., 1999
(1) Eastern Segment: North: Solør transect, Centre: Lake Vänern transect, South: South of Vårgårda, PZ: Protogine Zone
SFDZ: Sveconorwegian Frontal Deformation Zone
(2) Metamorphic facies: Am: amphibolite-facie, Gr: granulite-facies, Ecl: decompressed eclogite boudin
(3 | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_45.txt | 4 1.70 748 0.06993 33 1.47154 741 0.15261 29 926.4 9.5
(1) Number of crystals analysed
(2) Concentrations are known to ±30% for sample weights of 30 µg and ±50% for samples <3µg.
(3) Corrected for 0.0215 mole fraction common-Pb in the 205Pb-235U spike.
(4) Calculated Th/U ratio assuming that all 208Pb in excess of bla... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_67.txt | if ((0, n.Mt)(this.agentIdentifier, "distributed_tracing") && (r = (0, n.P_)(this.agentIdentifier).distributed_tracing), e.sameOrigin) t =!0;else if (r.allowed_origins instanceof Array) for (var i = 0; i < r.allowed_origins.length; i++) {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_29.txt | 1394 ±11 Andersson et al., 1999
South Folded metagranite dyke, Högabjär, HB3 Zrn U-Pb 1394 ±12 Möller et al., 2007
South Stensjö granite pegmatite dyke, 4 Zrn U-Pb 1399 +7/-6 Christoffel et al., 1999
South Varberg charnockite-granite association, 8 Zrn U-Pb 1399 +12/-8 Christoffel et al., 1999
South Glassvik deformed | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_113.txt | #onetrust-banner-sdk #onetrust-button-group-parent{width:100%;position:relative;margin-left:0}#onetrust-banner-sdk #onetrust-button-group button{display:inline-block}#onetrust-banner-sdk #onetrust-button-group{margin-right:0;text-align:center}#onetrust-banner-sdk.has-reject-all-button #onetrust-pc-btn-handler{float:lef... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1124.txt | differentiation likely took place in the upper crust."}],"$":{"view":"all","id":"spar0010"},"#name":"simple-para"}],"$":{"view":"all","id":"abst0010"},"#name":"abstract-sec"}],"$":{"view":"all","id":"abs0010","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"#name":"abstract... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_41.txt | detrital zircon clast.
(8) Figure presenting the concordia diagram
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 107 Table 2. ID-TIMS zircon U–Pb data. Fraction Concentrations Atomic ratios Age properties Wt. Pb U Pb Th/U 206Pb 207Pb ±
σ 207Pb ±
σ 206Pb ±
σ 207Pb ±
σ Disc
rad... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_75.txt | ower, C.F., Rivers, T. & Ryan, B.
(eds.), Mid-Proterozoic Laurentia-Baltica, 38, 149-173. Geological
Association of Canada, Special Paper 38.
Tucker, R.D., Ashwal, L.D., Handke, M.J., Hamilton, M.A., Le Grange,
M. & Rambeloson, R.A. 1999: U-Pb geochronology and isotope
geochemistry of the Archean and Proterozoic rocks | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_33.txt | zogranite Zrn U-Pb 1548 ±10 Lindh, 1996
PZ Åker metabasite Zrn U-Pb 1562 ±6 Söderlund et al., 2004
PZ Åker metabasite, dolerite dyke, 412 Zrn U-Pb 1567 ±3 Söderlund and Ask, 2006
Centre Metadolerite dyke, CHW670-OK450 Bdl U-Pb 1568 +30/-8 Wahlgren et al., 1996
Centre Öl | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1036.txt | _":"Hua-Feng"},{"#name":"surname","_":"Zhang"},{"#name":"cross-ref","$":{"refid":"af010","id":"c0075"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"b"}]},{"#name":"cross-ref","$":{"refid":"cor1","id":"c0080"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"⁎"}]},{"#name":"e-address","$":{"type":"email","id":"em005"},"_ | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_8.txt | ia is evaluated with zircon U-Pb geochronology. ID-TIMS,
LA-ICPMS and SIMS data are reported for 21 samples of orthogneiss, metarhyolite and metasandstone in S Norway, with emphasis on the Suldal
area. The Sveconorwegian orogen is divided into a reworked Fennoscandian 1.80-1.64 Ga parautochthonous segment, the Eastern ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1149.txt | Skar"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name":"surname","_":"Marker"}]},{"#name":"author","$$":[{"#name":"given-name","_":"E.M.O."},{"#name":"surname","_":"Sigmond"}]},{"#name":"author","$$":[{"#name":"given-name","_":"O."},{"#name":"surname","_":"Nordgulen"}]},{"#name":"author","$$":[{"# | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_62.txt |
Söderlund, P., Söderlund, U., Möller, C., Gorbatschev, R. & Rodhe, A.
2004: Petrology and ion microprobe U-Pb chronology applied to a
metabasic intrusion in southern Sweden: a study on zircon formation during metamorphism and deformation. Tectonics 23, TC5005,
doi:10.1029 /2003TC001498.
Söderlund, U. 1996: Conventiona... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_88.txt | B603, TB Am 207Pb/206Pb 1 901 ±7 Bingen & van Breemen, 1998
Telemark Drivheia granite gneiss, M200, Tb Am Low. intercept 4 907 ±14 Heaman & Smalley, 1994
Telemark Drivheia granite gneiss, M200, Tb Am 207Pb/206Pb 1 913 c. Heaman & Smalley, 1994
Telemark Fennefoss granodioritic augen gneiss, B613, TB Am 207 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_8.txt | ggrunnskart
Odda, 1:250000. Norges geologiske undersøkelse, Trondheim.
Sigmond, E.M.O., Birkeland, A. & Bingen, B. 2000: A possible basement to the Mesoproterozoic quartzites on Hardangervidda,
South-central Norway: zircon U-Pb geochronology of a migmatitic
gneiss. Norges geologiske undersøkelse Bulletin 437, 25- | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_81.txt | 66R Zrn U-Pb 1486 c. Pasteels & Michot, 1975
Suldal Ullensvang Gp, metarhyolite, S93-338 Zrn U-Pb 1489 ±1 Bingen et al., 2005
Suldal Skånevik supracrustals, metarhyolite, J-482A Zrn U-Pb 1491 ±5 Bingen et al., 2005
Telemark Granite gneiss, Gol, N95-112 Zrn U-Pb 1492 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1185.txt | aintitle","_":"The Sveconorwegian orogenic belt, a case of late-proterozoic plate-collision"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Geol. Rundsch."}]},{"#name":"volume-nr","_":"69"}]},{"#name":"date","_":"1980"}]},{"#name":"pages","$$":... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_29.txt | .G., Andersen, T. & Corfu, F. 2002: New
constraints on the timing of deposition and metamorphism in the
Bamble sector, south Norway: zircon and titanite U-Pb data from
the Nelaug area. GFF 124, 73-78.
Dons, J.A. 1960: Telemark supracrustals and associated rocks. In
Holtedahl, O., (ed.), Geology of Norway 208, 49-58. No... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_882.txt | ia, are below 0.14. Comparison between the Grenville Province in northeastern Laurentia and the Sveconorwegian Province in southwestern Fennoscandia (Baltica) shows some striking similarities, especially in the Mesoproterozoic, but also exhibits differences in the timing of events, especially during the final Grenville... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1173.txt | in Cordilleran orogenic systems"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Nat. Geosci."}]},{"#name":"volume-nr","_":"2"}]},{"#name":"date","_":"2009"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"251"},{"#name":"last-page","_":"25... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_40.txt | ation, SW Sweden. Geologiska Föreningens i Stockholm Förhandlingar 114, 461-462.
Lundqvist, T. & Persson, P.O. 1999: Geochronology of porphyries and
related rocks in northern and western Dalarna, south-central Sweden. GFF 121, 307-322.
Mansfeld, J. 2000: Abstract. 200 m.y. of episodic crustal growth in the
Østfold-Aker... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1401.txt | all the samples used for hornblende-plagioclase thermobarometry. (b) Pressure and temperature estimates for the SMB granites associated wit..."}]}],"extras":[],"attachments":[],"showEntitledTocLinks":false},"tail":{},"transientError":{"isOpen":false},"userAgent":"Mozilla/5.0 (Macintosh; Intel Mac OS X 10_15_7) AppleWe... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_18.txt | Pb 1603 ±40 Welin & Samuelsson, 1987
Migmatitic granodiorite, Stora Lundby, mesosome 9701b Zrn U-Pb 1605 ±10 Scherstén et al., 2004
Göteborg suite, Kallebäck orthogneiss Zrn U-Pb 1605 ±9 Åhäll & Connelly, 2008
Begna Granodioritic gneiss, Vindflomyra, N95-95 Zrn U-Pb 1606 ±2 Bingen et | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_54.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_785.txt | ft.volume=265C&rft.spage=57&rft.epage=77&rft.title=Precambrian%20Research&rft.atitle=The%20Late%20Mesoproterozoic%20Sirdal%20Magmatic%20Belt%2C%20SW%20Norway%3A%20Relationships%20between%20magmatism%20and%20metamorphism%20and%20implications%20for%20Sveconorwegian%20 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_284.txt | -cntr{padding-left:13px}#onetrust-pc-sdk.ot-pli-hdr~.ot-cat-item.ot-subgrp>h5,#onetrust-pc-sdk.ot-pli-hdr~.ot-cat-item.ot-cat-header{width:calc(100% - 145px)}#onetrust-pc-sdk.ot-pli-hdr~.ot-cat-item h5+.ot-tgl-cntr | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_32.txt | lower continental crust. Journal of Petrology
40, 909-933.
Korja, A., Lahtinen, R. & Nironen, M. 2006: The Svecofennian orogen: a collage of microcontinents and island arcs. In Gee, D.G. &
Stephenson, R.A. (eds.), European lithosphere dynamics. Geological
Society, London, Memoirs 32, 561-578.
Kullerud, L. & Machado, N... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_53.txt | iss Zrn 1250 ±22 Nordgulen et al., 1997
Bunketorp granite, 79023 Zrn 1279 ±62 Welin and Samuelsson, 1987
Støvika granite gneiss, Einavatnet Zrn 1280 +22/-14 Nordgulen et al., 1997
Ursand granite Zrn 1319 ±6 Piontek et al., 1998
Chalmers gabbro, felsic facies, DC9723 Zrn 1333 ±8 Kiel et al., 2003
Hästefj | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_20.txt | as the Falkenberg phase. Eclogite relics in the Eastern
Segment, dated at 972 ±14 Ma, attest to burial of Fennoscandia crust to a depth of at least 50 km. They represent the last undisputable evidence for convergence in
the Sveconorwegian belt, and their formation was shortly
followed by exhumation to a middle crustal ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_152.txt | -group{align-items:stretch;flex-direction:column-reverse;margin:0}div#onetrust-consent-sdk #onetrust-accept-btn-handler,div#onetrust-consent-sdk #onetrust-pc-btn-handler{flex:1 0 auto}}@media only screen and (min-width:768px){div#onetrust-banner-sdk #onetrust-policy{margin:0 48px 0 0}div#onetrust-consent-sdk #onetrust-... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1197.txt | #name":"title","$$":[{"#name":"maintitle","_":"Mid-Proterozoic Laurentia-Baltica: an overview of its geological evolution and a summary of the contributions made by this volume"}]}]},{"#name":"host","$$":[{"#name":"edited-book","$$":[{"#name":"editors","$$":[{"#name":"editor","$$":[{"#name":"given-name","_":"C.F."},{"#... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_62.txt | rocks
interlayered with immature clastic metasediments. These
rocks form several groups and formations of comparatively limited lateral extent. Local unconformities attest
to active erosion and tectonic activity between 1170 and
1140 Ma (Laajoki & Lamminen 2006). Geotectonic interpretation of the 1220-1130 Ma magmatis... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_81.txt | 24 3.13 0.27100 3.03 0.97 1503 15 1546 42 102.9
15a 226 65 67 18913 0.09398 0.59 3.2397 1.53 0.25003 1.41 0.92 1508 11 1439 18 95.4
09a 205 61 64 33220 0.09403 0.83 3.4070 3.14 0.26279 3.03 0.96 1509 16 1504 41 99.7
22a 97 38 30 13721 0.09473 0.79 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_69.txt | sdk-button,#onetrust-pc-sdk button,#ot-sdk-cookie-policy.ot-sdk-button,#ot-sdk-cookie-policy button{display:inline-block;height:38px;padding:0 30px;color:#555;text-align:center;font-size:.9em;font-weight:400;line-height:38px;letter-spacing:.01em;text-decoration:none;white-space:nowrap;background-color:rgba | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_24.txt | .0941 0.0010 3.07 0.05 0.237 0.003 0.72 1511 21 1370 14 90.7
9 0.0942 0.0009 3.46 0.07 0.266 0.005 0.89 1512 19 1522 26 100.7
7 0.0942 0.0013 3.37 0.06 0.259 0.003 0.60 1512 25 1486 13 98.3
12 0.0947 0.0014 3.32 0.07 0.254 0.004 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1023.txt | ":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]}],"floats":[],"footnotes":[],"attachments":[]},"title":{"content":[{"#name":"title","$":{"id":"tit0005"},"_":"High-temperature deformation in the basal shear zone of an eclogite-bearing fold nappe, Sveconorwegian orogen, Sweden"}],"floats":[],"footnotes":[],"attachments"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_435.txt | li:first-child{border-top:2px solid #b9b9b9}div#onetrust-pc-sdk.ot-host-item.ot-plus-minus{margin:0 8px 0 0}div#onetrust-pc-sdk.ot-search-cntr{width:calc(100% - 48px)}div#onetrust-pc-sdk.ot-host-opt.ot-host-info{background-color:transparent}div#onetrust-pc-sdk.ot | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_77.txt | le, O. & Duchesne, J.C. 2003: Derivation of the 1.0–0.9 Ga
ferro-potassic A-type granitoids of southern Norway by extreme
differentiation from basic magmas. Precambrian Research 124, 107-
148.
Verschure, R.H., Andriessen, P.A.M., Boelrijk, N.A.M., Hebeda, E.H.,
Maijer, C., Priem, H.N.A. & Verd | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_83.txt | et al., 2005
Suldal Sauda supracrustals, granodiorite gneiss, B00145 Zrn U-Pb 1497 ±12 Bingen et al., 2005
Suldal Botsvatn Co, Bykle, granodiorite gneiss, B02022 Zrn U-Pb 1498 ±8 Bingen et al., 2005
Suldal Granite gneiss, Vanvik, B00149 Zrn U-Pb 1499 ±11 Bingen et al., 2005
Suldal | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_3.txt | 22 99.4
5b 0.0934 0.0010 3.03 0.05 0.236 0.003 0.81 1496 20 1364 18 91.1
2c 0.0935 0.0006 3.27 0.05 0.254 0.004 0.91 1498 13 1458 19 97.3
7b 0.0937 0.0015 3.08 0.06 0.238 0.003 0.66 1503 29 1377 17 91.7
8a 0.0940 0.0008 3 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_646.txt | u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Nor. Geol. Unders. Bull.</h3></div><div class="series">(1998)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>T. </span>Falkum</span><em> et al.</em></span><h3 class="title">The ... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_4.txt | .21 0.06 0.247 0.004 0.90 1509 15 1425 21 94.5
11 0.0942 0.0014 3.15 0.07 0.243 0.004 0.77 1511 27 1400 22 92.6
3 0.0942 0.0014 3.01 0.06 0.232 0.003 0.69 1513 28 1345 17 88.9
B00-145, granodiorite gneiss, Sauda, Fig. 10C
4 0.0924 0.00 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_156.txt | - Type'
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