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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1085.txt | St Andrews KY16 9AL, UK"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Department of Earth and Environmental Sciences, University of St Andrews"},{"#name":"city","_":"St Andrews"},{"#name":"postal-code","_":"KY16 9AL"},{"#name":"country","_":"UK"}]}]},{"#name":"affiliation","$":{"id"... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1241.txt | "},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"A."},{"#name":"surname","_":"Möller"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P.J."},{"#name":"surname","_":"O’Brien"}]},{"#name":"author","$$":[{"#name":"given-name","_"... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_49.txt | ller, A., O'Brien, P.J., Kennedy, A. & Kröner, A. 2002: Polyphase
zircon in ultrahigh-temperature granulites (Rogaland, SW
Norway): constraints for Pb diffusion in zircon. Journal of
Metamorphic Geology 20, 727-740.
Möller, A., O'Brien, P.J., Kennedy, A. & Kröner, A. 2003: Linking
growth episodes of zircon and metamorp... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_743.txt | panel-title-text">Article Metrics</span></h2></span><svg focusable="false" viewBox="0 0 92 128" width="24" height="24" class="icon icon-navigate-down"><path d="m1 51l7-7 38 38 38-38 7 7-45 45z"></path></svg></button></header><div class="" aria-hidden="false" aria-describedby="metrics-header"><div class="plum-sciencedir... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_334.txt | always-active,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item.ot-acc-hdr.ot-always-active,#onetrust-pc-sdk #ot-pc-lst.ot-vs-list.ot-vnd-item.ot-acc-hdr.ot-always-active,#onetrust-pc-sdk.ot-accordion-layout.ot-checkbox-consent.ot-acc-hdr.ot-always-active{ | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_34.txt | racrustal rocks of the Dal group and late-Sveconorwegian
0.96-0.92 Ga granite plutons (Table 8, Fig. 7B).
Bamble-Kongsberg sector
The Bamble-Kongsberg sector forms a slightly warped
belt between the Telemark sector and the Idefjorden
terrane. It consists of amphibolite- to granulite-facies
para- and orthogneiss complex... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1370.txt | pdf":{"urlType":"download","url":"/science/article/pii/S0301926809002010/pdfft?md5=cc716e485becf4fd9f48db1dc56be99c&pid=1-s2.0-S0301926809002010-main.pdf"}},{"refId":30,"pii":"S0301926801001541","filesize":"897KB","pdf":{"urlType":"download","url":"/science/article/pii/S0301926801001541/ | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir2.txt | part2 -------------------
Oil field[edit]
An oil field with dozens of wells. This is the Summerland Oil Field, near Santa Barbara, California, before 1906
Eagle Ford Shale flares visible from space (green and infrared wavelengths), in the arc between "1" and "2", amid cities in southeast Texas in 2012.
An oil field is ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_690.txt | default" href="/science/article/pii/S0024493721003030"><span class="anchor-text">Evidence of crustal disequilibrium melting, mingling processes, layering and deformation in UHT conditions: The marginal zone of the Egersund-Ogna massif-type anorthosite (S. Norway)</span></a></h3><div class="text-s">2021, Lithos</div></d... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_31.txt | },
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_3.txt | 40 Ma has been detected in the Bamble Terrane
in the Arendal area. The orogenic phase associated with
this metamorphism is thus referred to as the Arendal
phase (Fig. 8a). This phase is best interpreted as an earlySveconorwegian 1140-1080 Ma collision between the
Telemarkia and Idefjorden Terranes (Figs. 8a, 9). This
c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_453.txt | -cookie-policy-v2.ot-sdk-cookie-policy table tr:last-child td{border-bottom:0px}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table tr th:last-child,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table tr td:last-child{border-right:0px}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy table.ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1380.txt | -highlights","depth":"1"},"$$":[{"#name":"title","$":{"id":"sect0005"},"_":"Highlights"}]},{"#name":"entry","$":{"id":"abs0010","type":"abstract","class":"author","depth":"1"},"$$":[{"#name":"title","$":{"id":"sect0010"},"_":"Abstract"}]},{"#name":"entry","$":{"id":"kwd0005","type":"keywords","class":"keyword","depth":... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_68.txt | 1271-1247 Ma Central Scandinavian Dolerite Group which occurs over large parts
of Fennoscandia (Söderlund et al. 2006). The 1220-1190
Ma granite plutonism in the Telemark Sector (Heaman
& Smalley 1994; Andersen et al. 2007b) is coeval with
the 1220-1200 Ma, mainly granitic plutonism along the
Protogine Zone (Larsson &... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_9.txt | segment, Hisingen suite, Bot granite Zrn U-Pb 1541 ±11 Åhäll & Connelly, 2008
Koster segment, Hisingen suite, Måskär granite Zrn U-Pb 1545 ±5 Åhäll & Connelly, 2008
Ranrike granodiorite east Zrn U-Pb 1546 ±4 Åhäll & Connelly, 2008
Koster segment, Storön tonalite Zrn U-Pb 1546 ±7 Åhäll | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_28.txt | ism largely overlaps the formation of the second
and third phases of the Transscandinavian Igneous
Belt, representing the foreland of the Sveconorwegian
orogen (Åhäll & Larson 2000; Andersson et al. 2004).
Consequently, the Eastern Segment is interpreted as a
part of the Transscandinavian Igneous Belt that was
underthr... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_118.txt | T: () => u
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_39.txt | . Isotopic
arguments (Andersen et al. 2001; Andersen et al. 2002b)
and provenance analysis of detrital zircons (Knudsen et al.
1997; de Haas et al. 1999; Bingen et al. 2001a) are compatible with restoration of Telemarkia at the margin of Fennoscandia. Such a restoration is consistent with a simple
geographic polarity f... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_795.txt | 31649ea5c81fa189gxrqa%7C%24%7C9A361342D5830378190D3D7AFF9457691EF0BE933086A4258E4D7FB42E5CDA3EC3BE1A2AD34978E6E467FBA88B160B471687035859AC27543FBA44D1BD4E4F2EB0469A67597464825D387A21AFA2E514&utt=eed1 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_684.txt | -bottom u-font-serif text-s" id="reference-abstract"><div class="u-margin-ver-m"><p id="sp0015">A total of 4344 magmatic U-Pb ages in the range 2300 to 800 Ma have been compiled from the Great Proterozoic Accretionary Orogen along the margin of the Columbia / Nuna supercontinent and from the subsequent Grenvillian... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_45.txt | en et al. 2006). Titanite U-Pb data define a regional scale
cluster at 918 ±2 Ma, best regarded as a cooling age (Fig.
4, Table 5; Bingen & van Breemen 1998b). Amphibole
40Ar/39Ar apparent ages range from 1059 ±8 to 853 ±3
Ma (Bingen et al. 1998). The main cluster at 871 ±10 Ma
overlaps with biotite Rb-Sr ages (Verschu... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1028.txt | _":"Abstract"},{"$$":[{"$$":[{"#name":"__text__","_":"Ductile shear zones associated with emplacement of high-pressure nappes are key features to resolve exhumation mechanisms. The Eastern Segment of the Sveconorwegian orogen hosts an eclogite-bearing fold nappe, whose basal shear zone shows structures associated with ... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_25.txt | N. & Åhäll, K.-I. 1996: The Mesoproterozoic cratonization
of Baltica - new age constraints from SW Sweden. In Brewer, T.S.
(ed.), Precambrian crustal evolution in the North Atlantic Region,
112, 261-273. Geological Society of London, Special Publications.
Cornell, D.H. & Austin Hegardt, E. 2004: Abstract. When, where a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_949.txt | matism"},{"#name":"para","$":{"id":"par0355","view":"all"},"$$":[{"#name":"__text__","_":"The metamorphic evolution of SW Norway has generally been ascribed to a ca. 1035–970"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"Ma (Bingen et al., 2008a) regional event, followed by a younger, contact-metamorphic... | |
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no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir4.txt | part4 -------------------
Formation[edit]
Crude oil is found in all oil reservoirs formed in the Earth's crust from the remains of once-living things. Evidence indicates that millions of years of heat and pressure changed the remains of microscopic plants and animals into oil and natural gas.
Roy Nurmi, an interpretati... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_222.txt | rust-pc-sdk #filter-btn-handler{background-color:#3860be;border-radius:17px;display:inline-block;position:relative;width:32px;height:32px;-moz-transition:.1s ease;-o-transition:.1s ease;-webkit-transition:1s ease;transition:.1s ease;padding:0;margin:0}#onetrust-pc-sdk #filter-btn-handler:hover{background-color:#3860 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_999.txt | 1-s2.0-S0301926814002514-fx1.jpg"},{"#name":"ucs-locator","_":"https://s3.amazonaws.com/prod-ucs-content-store-us-east/content/pii:S0301926814002514/fx1/DOWNSAMPLED/image/jpeg/b9d097a308ec5c15c713b6018ac83cf8/fx1.jpg"},{"#name":"ucs-locator"," | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_73.txt | rn 1051 +2/-8 Bingen and van Breemen, 1998 a
Feda augen gneiss suite, Feda, B113 R Zrn 1051 +2/-8 Bingen and van Breemen, 1998 a
Feda augen gneiss suite, Liland, B195 R Zrn 1051 +2/-4 Bingen and van Breemen, 1998 a
Morkheia monzonite suite, M220 T Zrn 1134 ±2 Heaman and Smalley, 1994
Gunnarstul granite gneiss T | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_17.txt | ia Terrane (Andersson et al. 1996; Ebbing et al.
2005). The Kongsberg Terrane shows a steep, N-S trending Sveconorwegian structural grain (Starmer 1985;
Andersen & Munz 1995). Peak amphibolite-facies conditions are in the sillimanite stability field (Munz 1990).
The Bamble Terrane has a pronounced NE–SW trending
struct... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_70.txt | 113 Zrn U-Pb 1051 +2/-8 Bingen & van Breemen, 1998
Rogaland Feda granodiorite suite, Liland augen gneiss, B195 Zrn U-Pb 1051 +2/-4 Bingen & van Breemen, 1998
Suldal Garnet granite gneiss, Vanvik, B00147 Zrn U-Pb 1065 ±74 Bingen et al., 2005
Telemark Morkheia monzonite suite, monzonite M37 Zrn U-Pb 11 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_147.txt | -policy-text,div#onetrust-consent-sdk #onetrust-policy-text{font-size:16px;line-height:24px;max-width:44em;margin:0}div#onetrust-consent-sdk #onetrust-policy-text a[href]{font-weight:400;margin-left:8px}div#onetrust-banner-sdk #onetrust-button-group-parent{flex:0 0 auto;margin:32px 0 0;width:100% | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_80.txt | central Sweden. Precambrian Research
70, 67-91.
Walderhaug, H.J., Torsvik, T.H., Eide, E.A., Sundvoll, B. & Bingen, B.
1999: Geochronology and palaeomagnetism of the Hunnedalen
dykes, SW Norway: implications for the Sveconorwegian apparent
polar wander loop. Earth and Planetary Science Letters 169, 71-83.
Wang, X.D., S... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_54.txt | are
common and locally very abundant. The granite is metaluminous to weakly peraluminous with limited variation
in composition as shown, for example, by a narrow range
in SiO2
(69-74 wt%) and K2
O (4.2-5.8 wt%) contents
(Nordgulen, unpublished data).
Sample N94-38 is a biotite granite collected in the southern margin... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_62.txt | i = c(t),
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_112.txt | Söderlund et al. 1999; Johansson et al. 2001). The main group of hornblende 40Ar/39Ar
plateau ages between 934 ±6 and 931 ±6 Ma, from the
southern part of the segment, is interpreted by Page et al.
(1996a; 1996b) as the timing of cooling through c. 550-
500 °C.
Around and south of lake Vänern, the Eastern Segment
is c... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_940.txt | is crucial to understand the regional geologic evolution, as SMB granitoids can be used as time markers. In the following section we describe in detail the nature of the host rocks and their contacts with the SMB, focusing on the western and southwestern part of the SMB."},{"#name":"section","$":{"id":"sec0090","view"... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1191.txt | #name":"editor","$$":[{"#name":"given-name","_":"J.L.R."},{"#name":"surname","_":"Touret"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The Deep Proterozoic Crust in the North Atlantic Provinces"}]},{"#name":"date","_":"1985"},{"#name":"publisher","$$":[{"#name":"name","_":"Reidel"},{"#name":"location","_":"Dor... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_34.txt | uture zone in the
Sveconorwegian belt, if any, is between the Telemarkia
and Idefjorden Terranes. This interpretation implies that
the Telemarkia Terrane was possibly exotic to Fennoscandia, and accreted during the Sveconorwegian orogeny, by
closure of an oceanic basin (Figs. 7, 9).
The four Sveconorwegian orogenic pha... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1344.txt | ":"date","_":"1990"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"33"},{"#name":"last-page","_":"50"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0345"},"$$":[{"#name":"label","_":"Westphal et al., 2003"},{"#name":"reference","$":{"id":"sbref0345","refId":"69"},"$$":[{"#name":"contribution","$":{"langtype":"e... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_11.txt | 539-552.
Dahlgren, S., Heaman, L. & Krogh, T. 1990: Abstract. Geological evolution and U-Pb geochronology of the Proterozoic Central Telemark
area, Norway. Geonytt 17, 38-39.
de Haas, G.J.L.M., Andersen, T. & Vestin, J. 1999: Detrital zircon
geochronology: new evidence for an old model for accretion of the
SW Baltic S... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_788.txt | Elsevier B.V. All rights reserved.","cover-date-years":["2015"],"cover-date-start":"2015-08-01","cover-date-text":"August 2015","document-subtype":"fla","document-type":"article","eid":"1-s2.0-S0301926815001424","doi":"10.1016/j.precamres.2015.05.002","first-fp":"57","hub-eid":"1-s2.0-S0301926815X00088","issuePii":" | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_2.txt | er & Smeds, 1996
Skantorp rare-mineral pegmatite Clm U-Pb 1041 ±2 Romer & Smeds, 1996
Sandsjön granite gneiss, 78140 Zrn U-Pb 1210 +36/-34 Welin et al., 1981
Segmon granite, SWS9 Zrn U-Pb 1249 +10/-7 Persson et al., 1983
Bunketorp granite, 79023 Zrn U-Pb 1279 ±62 Welin & Samuelsson, 1987
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1363.txt | "},{"refId":58,"scopusHubEid":"2-s2.0-0030513461"},{"refId":59,"crossRefDoi":"10.1007/978-94-009-5450-2_28"},{"refId":60,"scopusHubEid":"2-s2.0-20444466409","crossRefDoi":"10.1111/j.1525-1314.2005.00572.x"},{"refId":62,"scopusHubEid":"2-s2.0-00414618 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_32.txt | Idefjorden
terrane included accretion of juvenile oceanic arcs to
the continent between 1.66 and 1.52 Ga. As argued by
Cornell and Austin Hegardt (2004), no magmatic suite
overlaps between the Idefjorden terrane and the
Eastern Segment. The Idefjorden terrane can thus be
alternatively interpreted as an exotic terrane ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_465.txt | 2.ot-sdk-cookie-policy h6,
#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy li,
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_995.txt | label","_":"1"},{"#name":"note-para","$":{"id":"npar0020","view":"all"},"_":"Tel.: +1 416 946 7424."}]}]}],"floats":[],"footnotes":[{"#name":"footnote","$":{"id":"fn0005"},"$$":[{"#name":"label","_":"1"},{"#name":"note-para","$":{"id":"npar0020","view":"all"},"_":"Tel.: +1 416 946 7424."}]}],"attachments":[]},"lastAuth... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_1.txt | Fig. 12 are permissible. The
first model restoring Telemarkia to the margin of an exotic craton before the Sveconorwegian orogeny implies a
collision event lasting 160 m.y. The second model restoring Telemarkia to the margin of Fennoscandia features
two collisions with closure of an oceanic basin: a first
collision be... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_5.txt | WSW Danopolonian shortening. International Journal of
Earth Sciences 96, 397-414.
Christoffel, C.A., Connelly, J.N. & Åhäll, K.I. 1999: Timing and characterization of recurrent pre-Sveconorwegian metamorphism and
deformation in the Varberg–Halmstad region of SW Sweden. Precambrian Research 98, 173-195.
Claeson, D.T. 19... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_16.txt | Tables 1, 5; Figs. 10I, J). These two samples
contain zircon xenocrysts with ages of 1508 ± 32 and
1494 ± 33 Ma. One of these (B00-147) is a leucocratic
garnet-bearing rock collected in an inhomogeneous
outcrop in the gneiss complex, and probably corresponds to a granitic melt of local origin. Although
imprecise, the ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_33.txt | video.position = parseFloat(data.video.position || '0');
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_27.txt | zoic
Oslo rift. It is bounded by the Mylonite Zone to the east
and by the Östfold-Marstrand and Åmot-Vardefjell
Shear Zones to the west (Figs. 1, 2; Åhäll et al. 1998;
Bingen et al. 2001a). An amphibolite-rich, banded
paragneiss complex limits the terrane along the
Åmot-Vardefjell Shear Zones. The terrane comprises
gre... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_417.txt | 24px}div#onetrust-consent-sdk #onetrust-pc-sdk p,div#onetrust-pc-sdk #ot-pc-desc,div#onetrust-pc-sdk.category-host-list-handler,div#onetrust-pc-sdk.ot-accordion-layout.ot-cat-header{font-size:16px;font-weight:400;line-height:24px}div#onetrust-consent-sdk a:hover,div#onetrust- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_296.txt | ot-pgph-desc:not(:last-child):after{content:"";width:96%;display:block;margin:0 auto;padding-bottom:2rem;border-bottom:1px solid #e9e9e9}#onetrust-pc-sdk.ot-cat-header{float:left;font-weight:600;font-size:.875em;line-height:1.5;max-width:90%;vertical-align:middle}#onetrust-pc-sdk.ot-v | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_12.txt | 569-586.
de Haas, G.J.L.M., Nijland, T.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.
B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
69
Demaiffe, D., Weis, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_759.txt | Opens in new window" width="1em" height="1em" class="icon icon-arrow-up-right arrow-external-link"><path d="m4 36h57.07l-59.5 59.5 7.07 7.08 59.36-59.36v56.78h1e1v-74h-74z"></path></svg></a></li><li><a class="anchor u-display-block u-clr-grey8 u-margin-s-bottom u-margin-0- | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_30.txt | se.
Duchesne, J.-C., Liégeois, J.-P., Vander Auwera, J. & Longhi, J. 1999:
The crustal tongue melting model and the origin of massive
anorthosites. Terra Nova 11, 100-105.
Ebbing, J., Afework, Y., Olesen, O. & Nordgulen, Ø. subm: Is there
evidence for magmatic underplating beneath the Oslo rift? Terra
Nova.
Eliasson, T... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_191.txt | onetrust-pc-sdk ul.ot-subgrps{margin:0;font-size:initial}#onetrust-pc-sdk ul.ot-subgrps li p,#onetrust-pc-sdk ul.ot-subgrps li h5{font-size:.813em;line-height:1.4;color:dimgray}#onetrust-pc-sdk ul.ot-subgrps.ot-switch{min-height:auto}#onetrust-pc-sdk ul. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_65.txt | und, G., Heaman, L.M., Patchett, P.J.,
Vervoort, J.D. & Andersson, U.B. 2005: U-Pb baddeleyite ages, and
Hf, Nd isotope chemistry constraining repeated mafic magmatism
in the Fennoscandian Shield from 1.6 to 0.9 Ga. Contributions to
Mineralogy and Petrology 150, 174-194.
Söderlund, U. & Ask, R. 2006: Evidence for two | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1181.txt | ":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Nor. Geol. Unders."}]}]},{"#name":"date","_":"1982"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0095"},"$$":[{"#name":"label","_":"Falkum, 1998"},{"#name":"reference","$":{"id":"sbref0095","refId":"19"},"$$":[{"#name":"contribution","$":{"l... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1494.txt |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_40.txt | /-8 Christoffel et al., 1999
Glassvik deformed pegmatite dyke Zrn 1409 ±20 Söderlund, 1996
Särdal granite pegmatite dyke, S3 Zrn 1426 +9/-4 Christoffel et al., 1999
Gåsanabbe mafic orthogneiss, S5 Zrn 1438 +12/-8 Christoffel et al., 1999
Gällared S deformed granite-aplite dyke Zrn 1443 ±26 Söderlund et al., 2002 | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_50.txt | M.B. & Wahlgren, C.H. 1996b: 40Ar/39Ar geochronological constraints on the tectonothermal evolution of the Eastern Segment of the Sveconorwegian Orogen, south-central Sweden. In Brewer, T.S. (ed.), Precambrian crustal evolution in the North
Atlantic Region. Geological Society, London, Special Publications
112, 315-330... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_18.txt | .J. & Austrheim, H. 2001b: Zircon U-Pb geochronology in the Bergen Arc eclogites and their Proterozoic protoliths,
and implications for the pre-Scandian evolution of the Caledonides
in western Norway. Geological Society of America Bulletin 113,
640-649.
Bingen, B., Mansfeld, J., Sigmond, E.M.O. & Stein, H.J. 2002: Balt... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_50.txt | utons (Table 10).
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 93
Fig. 6. (A) Cathodoluminescence image of zircon 01 of sample B00-
140, showing a typical oscillatory zoning of magmatic origin. (B)
Optical image of the same crystal after analysis, showing the size of a
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_580.txt | !-- -->Ma was local rather than regional in SW Norway.</p><p id="spar0025">The orogenic evolution of SW Norway is characterized by emplacement of large volumes of granitic magma and more localized UHT metamorphism, which is quite different from the widespread, long-lasting metamorphic evolution observed in the Grenvill... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_115.txt |
to extensional deformation at 949 ±4 Ma at the Vistbergen locality (Fig. 4; Connelly et al. 1996).
The Eastern Segment is bounded in the east by two orogen-parallel lineaments, the Protogine Zone and the
Sveconorwegian Frontal Deformation Zone (SFDZ; Fig.
1; Andréasson & Rodhe 1990; Wahlgren et al. 1994). The
Protogin... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_513.txt | 9.05zm80.33 29.6l-26.32-26.32c5.61-7.15 8.68-15.9 8.68-25.13 0-10.91-4.25-21.17-11.96-28.88-7.72-7.71-17.97-11.96-28.88-11.96s-21.17 4.25-28.88 11.96c-7.72 7.71-11.97 17.97-11. |
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