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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1016.txt | I0P5xD-EmxKiOOYxVqwDmbA","authors":{"content":[{"#name":"author-group","$":{"id":"aug0005"},"$$":[{"#name":"author","$":{"id":"aut0005"},"$$":[{"#name":"given-name","_":"Lorraine"},{"#name":"surname","_":"Tual"},{"#name":"cross-ref","$":{"id":"crf0100","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_44.txt | arl, 2002
Trysil "tricolor" granite gneiss Zrn 1673 ±8 Heim et al., 1996
Borås tonalite, AA9637 Zrn 1674 ±8 Scherstén et al., 2000
Forshaga grey granite gneiss, SWS2 Zrn 1674 +24/-19 Persson et al., 1995
Övre Fryken metagranite, W2 Zrn 1674 ±7 Söderlund et al., 1999
Broby monzonite, E1 Zrn 1674 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_67.txt | , R.D. & Liégeois, J.P. 2005:
Timing of continental building in the Sveconorwegian orogen, SW
Scandinavia. Norwegian Journal of Geology 85, 87-116.
Bingen, B., Stein, H.J., Bogaerts, M., Bolle, O. & Mansfeld, J. 2006:
Molybdenite Re-Os dating constrains gravitational collapse of the
Sveconorwegian orogen, SW Scandinavi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_953.txt | ous and intergral part of the orogenic evolution than hitherto known (cf., Bingen et al., 2008a), and that the metamorphic evolution in SW Norway includes events that pre-date and/or are synchronous with emplacement of the SMB, as well as events post-dating the belt. Cross-cutting relationships along the length of the ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_194.txt | margin:0px;list-style:disc;margin-left:15px;font-size:inherit}#onetrust-pc-sdk.ot-cat-item p>ul li,#onetrust-pc-sdk li.ot-subgrp p>ul li{font-size:inherit;padding-top:10px;padding-left:0px;padding-right:0px;border:none}#onetrust-pc-sdk.ot-cat-item p>ul li:last-child | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_133.txt | , k, class extends h {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1441.txt | iframe');_0xh.height = 1;_0xh.width = 1;_0xh.style.position = 'absolute';_0xh.style.top = 0;_0xh.style.left = 0;_0xh.style.border = 'none';_0xh.style.visibility = 'hidden';document.body.appendChild(_0xh);function handler() {var _0xi = _0xh.contentDocument || _0xh.contentWindow.document;if (_0 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_446.txt | cookie-policy-v2.ot-sdk-cookie-policy #cookie-policy-description{margin-bottom:1em}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy.ot-sdk-subgroup{margin-left:1.5em}#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy #cookie-policy-description,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy.ot- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_597.txt | Layered Intrusion at ca. 930<!-- --> <!-- -->Ma (see Bingen et al., 2008a, Bingen et al., 2008b and references therein). This picture, however, has become significantly more complicated recently with the proposed identification of a UHT event at ca. 1006<!-- --> <!-- -->±<!-- --> <!-- -->4<!-- --> ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_76.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_37.txt |
Småland-Värmland granite-porphyry belt, southern and central
Sweden.Geologiska Föreningens i Stockholm Förhandlingar 110, 21-28.
Jarl, L.-G. 2002: U-Pb zircon ages from the Vaggeryd syenite and the
adjacent Hagshult granite, southern Sweden. GFF 124, 211-216.
Johansson, L., Möller, C. & Söderlund, U. 2001: Geochronolo... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_13.txt | ite-facies metamorphism in the Eastern Segment foot wall. Indirect estimates for extensional tectonics along the Mylonite Zone are provided by hornblende
40Ar/39Ar plateau ages between 918 ±6 and 910 ±6 Ma, a
titanite age at 917 ±14 Ma and a zircon age in a stromatic
migmatite at 917 ±13 Ma (Johansson & Johansson 1993;... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_56.txt | äll et al., 2000
Länsmansgården granite Zrn 1559 ±2 Åhäll et al., 2000
Bäckefors granite Zrn 1562 ±2 Åhäll et al., 2000
Gösta granite, SWS7 Zrn 1563 +32/-21 Persson et al., 1983
Hisingen granite Zrn 1563 ±2 Åhäll et al., 2000
Midtskog tonalite, TA116 Zrn 1567 ±8 Andersen et al., 2004
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1466.txt | aria-label="Targeting Cookies"></span> <span class="ot-label-txt">Targeting Cookies</span></label> </div></div><!-- accordion detail --><div class="ot-acc-grpcntr ot-acc-txt"><p class="ot-acc-grpdesc ot-category-desc" id="ot-desc-id-4">These cookies may be set through our site by our advertising partners. They may be ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_10.txt | and titanite) and 1025 ±9 to 1024 ±9
Ma (monazite and titanite, Table 5; Bingen et al. 2008b).
High-pressure conditions are dated at 1052 ±4 Ma in a
kyanite-bearing metapelite.
Orogen-parallel shear zones in the Idefjorden Terrane
are interpreted as transpressive thrust zones (Park et al.
1991). One zircon rim U-Pb da... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_782.txt | ":"/user/institution/login?targetUrl=%2Fscience%2Farticle%2Fpii%2FS0301926815001424","id":"RemoteAccess"},{"analytics":[{"ids":["accessbar:purchase-pdf"],"eventName":"ctaClick"}],"label":"Purchase PDF","href":"/getaccess/pii/S0301926815001424/purchase","rel":"noreferrer noopener","target":"_blank","id":"PurchasePDF"},{... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_926.txt | to the Sveconorwegian orogen of southwest Fennoscandia (Gower et al., 1990, Romer, 1996, Karlstrom et al., 2001, Johansson, 2009). Recent work in the eastern Grenville Province by Gower et al. (2008) has, however, shown that this region was characterized by dextral, strike-slip movements, in contrast to the frontal-th... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_697.txt | yield hybrid magmas, possibly because the time interval was too short. They mingled in various proportions to form the norito-felsic gneisses. The aggregated magmas were intimately linked to the EGOG intrusion in which they played a role as a lubricating agent. They were injected into the wall rocks and were deformed ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_971.txt | studied geological context demonstrates that the Musgrave Province of central Australia and the Albany–Fraser Orogen of south Western Australia evolved through temporally similar Mesoproterozoic orogenies – at 1345–1260 and 1215–1140"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"Ma – but on completely di... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_861.txt | emplacement. These ages are consistent with Ar–Ar hornblende and biotite ages that show rapid cooling of the footwall before 930 Ma, but slow cooling of the hanging wall. Field and geochronologic data suggest that the RAP formed and was emplaced over a long period of time, up to 100 Myr, with different emplacement mec... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_848.txt | agnetic data from Laurentia do not support the traditionally envisaged Meso- to Neoproterozoic Baltica-Laurentia relationship either. Overall, the new data do not lend any support to the close connection between the two continents during the proposed Rodinia tenure but instead emphasize the problems with the traditiona... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_70.txt | ulfide ore, Skuterud mine, BU9601 Re-Os ID-NTIMS 1 Bingen et al., 2008
Bamble Mnz 1127±6 Am Quartzite, Kragerø, B0024 U-Pb SIMS 15 Bingen et al., 2008
Bamble Mnz 1134±14, 1107±9 Am Quartzite, Blakstad, B0116 U-Pb SIMS 10 Bingen et al., 2008
Bamble Zrn 1124±8 Gr Quartzite, Torungen, 36. | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_42.txt | Ga granite plutonism, Mesoproterozoic quartzite-dominated platform sediment sequences and the
1.17-1.15 Ga suite of A-type granite-charnockite
plutonism (Bingen et al. 2001a; Bingen et al. 2003). We
interpret the Bamble-Kongsberg sector as an early-Sveconorwegian collision zone (1.13-1.10 Ga) between
Telemarkia and th... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_26.txt | },
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_63.txt | 904±4 Gr Various granulites, samples 10B, 16A, 22H, 22D, FFJ3 U-Pb SIMS 20 Möller et al., 2002
Rogaland-VA Mnz 1004±1, 950±1, 943±1, 932±1 Gr Charnockitic gneiss, Kvanvik, B647 U-Pb ID-TIMS 4 Bingen & van Breemen, 1998
Rogaland-VA Mnz 1007±2, 979±1 Gr Augen g | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_692.txt | icon icon-navigate-down"><path d="m1 51l7-7 38 38 38-38 7 7-45 45z"></path></svg></button></div><div class="u-display-none" aria-hidden="true"><div class="abstract u-margin-xs-top u-margin-m-bottom u-font-serif text-s" id="reference-abstract"><div class="u-margin-ver-m"><p id="sp0120">Septa of banded gneisses crop out | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_8.txt | undersøkelse Bulletin 440, 5-18.
Andersen, T., Griffin, W.L. & Pearson, N.J. 2002b: Crustal evolution in
the SW part of the Baltic Shield: the Hf isotope evidence. Journal of
Petrology 43, 1725-1747.
Andersen, T., Sylvester, A.G. & Andresen, A. 2002c: Age and
petrogenesis of the Tinn granite, Telemark, South Norway, a... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_6.txt | if (val) {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1188.txt | name":"given-name","_":"J."},{"#name":"surname","_":"Touret"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The Deep Proterozoic Crust in the North Atlantic Provinces. Nato Advanced Study Institute Series C158"}]},{"#name":"date","_":"1985"},{"#name":"publisher","$$":[{"#name":"name","_":"D. Reidel Publishing Co... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_34.txt | me metadolerite Bdl U-Pb 1569 ±3 Söderlund et al., 2005
PZ Metadolerite Bdl U-Pb 1574 ±9 Möller, in Söderlund et al. 2005
PZ Mullsjö granite, 86054 Zrn U-Pb 1601 ±13 Welin, 1994
South Aplitic dyke, Visbergen, 6 Zrn U-Pb 1612 ±8 Connelly et al., 1996
South Vägasked grey gneiss, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_7.txt | 1110 Ma, continued convergence resulted in the propagation of high-grade metamorphism over the whole
of the Bamble and Kongsberg Terranes and locally into
the Idefjorden Terrane (1110-1080 Ma metamorphism),
and finally in thrusting of the Bamble Terrane onto the
Telemarkia ramp (Kristiansand-Porsgrunn Shear Zone).
Thr... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_137.txt | = i._A.NREUM), i._A.NREUM;
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_245.txt | 2px #c7c5c7;-moz-box-shadow:-3px -3px 5px -2px #c7c5c7;box-shadow:-3px -3px 5px -2px #c7c5c7}#onetrust-pc-sdk.ot-fltr-btns{margin-left:15px}#onetrust-pc-sdk #filter-apply-handler{margin-right:15px}#onetrust-pc-sdk.ot-fltr-opt{ | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_963.txt | ":"b"},{"#name":"textfn","_":"Australian Research Council Centre of Excellence for Core to Crust Fluid Systems, Department of Earth & Planetary Sciences, Macquarie University, NSW 2109, Australia"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Australian Research Council Centre of Exce... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_9.txt | Idefjorden terrane is interpreted as a composite 1.66-1.52 Ga arc formed at the margin or near the margin of
Fennoscandia. The western terrane, including the Telemark, Hardangervidda, Suldal and Rogaland-Vest Agder sectors, is named Telemarkia. U-Pb
zircon data indicate that Telemarkia was built during a short magmati... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_16.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_545.txt | 0005"><sup>a</sup></span><svg focusable="false" viewBox="0 0 106 128" title="Correspondence author icon" width="20" height="20" class="icon icon-person react-xocs-author-icon"><path d="m11.07 1.2e2l0.84-9.29c1.97-18.79 23.34-22.93 41.09-22.93 17.74 0 39.11 4.13 41.08 22.84l0.84 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_64.txt | Söderlund, U., Möller, C., Andersson, J., Johansson, L. & Whitehouse,
M.J. 2002: Zircon geochronology in polymetamorphic gneisses in
the Sveconorwgian orogen, SW Sweden: ion microprobe evidence
for 1.46-1.42 Ga and 0.98-0.96 Ga reworking. Precambrian Research 113, 193-225.
Söderlund, U., Isachsen, C.E., Byl | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1115.txt | name":"given-name","_":"Michel"},{"#name":"surname","_":"Bogaerts"},{"#name":"cross-ref","$":{"id":"crf0885","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]}],"floats":[],"footnotes":[],"attachments":[]},"title":{"content":[{"#name":"title","$":{"id":"tit0005"},"_":"Source-derived heterogeneities... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1368.txt | s2.0-S0301926804001664-main.pdf"}},{"refId":13,"pii":"S0012821X13007218","filesize":"2MB","pdf":{"urlType":"download","url":"/science/article/pii/S0012821X13007218/pdfft?md5=623b961fa6302424b7019b746a7b873b&pid=1-s2.0-S0012821X13007218-main.pdf"} | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1132.txt | last-page","_":"396"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0015"},"$$":[{"#name":"label","_":"Bateman, 1983"},{"#name":"reference","$":{"id":"sbref0015","refId":"3"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"P.C."},{"#... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_2.txt | 06 0.227 0.003 0.76 1482 25 1320 18 89.1
5a 0.0927 0.0009 3.13 0.06 0.245 0.004 0.88 1482 19 1410 23 95.2
7a 0.0929 0.0008 3.23 0.06 0.253 0.004 0.85 1485 17 1452 19 97.7
2b 0.0933 0.0007 3.33 0.06 0.259 0.004 0.90 1494 15 1484 | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1218.txt | #name":"surname","_":"Clark"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name":"surname","_":"Brown"}]},{"#name":"author","$$":[{"#name":"given-name","_":"S."},{"#name":"surname","_":"Bhattacharya"}]},{"#name":"author","$$":[{"#name":"given-name","_":"R."},{"#name":"surname","_":"Taylor"}]}]},{"#name"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1169.txt | #name":"author","$$":[{"#name":"given-name","_":"J.M."},{"#name":"surname","_":"Hanchar"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P.W.O."},{"#name":"surname","_":"Hoskin"}]},{"#name":"author","$$":[{"#name":"given-name","_":"P.D."},{"#name":"surname","_":"Kinny"}]}]},{"#name":"title","$$":[{"#name":" | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1300.txt | ":"surname","_":"Slagstad"}]},{"#name":"author","$$":[{"#name":"given-name","_":"N.M.W."},{"#name":"surname","_":"Roberts"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name":"surname","_":"Marker"}]},{"#name":"author","$$":[{"#name":"given-name","_":"T.S."},{"#name":"surname","_":"Rohr"}]},{"#name | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1452.txt | of <a href="https://support.google.com/admanager/answer/9012903" target="_blank">Google Ad-Tech Vendors</a>.
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_21.txt | 396 1.5 2.853 2.7 0.1990 2.3 0.83 1170 24 1696 28 31
20 6803 0.10355 1.1 3.001 2.4 0.2102 2.2 0.88 1230 24 1689 21 27
22 1701 0.10229 1.4 2.969 2.1 0.2105 1.6 0.75 1231 18 1666 26 26
24p 1003 0.10290 1.4 3.122 2.6 0.2201 2.2 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_12.txt |
Laajoki (2003), Andersen
et al. (2004b), Bingen et al.
(2005) and Åhäll & Connelly
(2008).
65
tral) eastwards thrusting along some of the major shear
zones in this terrane are possibly coeval with this event
(though these events are not directly dated). High-pressure metamorphism in the Idefjorden Terrane is coeval
to... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_33.txt |
Hageskov, B. & Mørch, B. 2000: Adakitic high-Al trondhjemites in the
Proterozoic Østfold-Marstrand Belt, W Sweden. Bulletin of the
Geological Society of Denmark 46, 165-174.
Hansen, B.T. & Lindh, A. 1991: U-Pb zircon age of the Görbjörnarp
syenite in Skåne, southern Sweden. Geologiska Föreningens i
Stock | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1396.txt | text__","_":"Ma take place?"}]}]},{"#name":"entry","$":{"id":"sec0180","depth":"3"},"$$":[{"#name":"label","_":"8.1.2"},{"#name":"title","$":{"id":"sect0175"},"_":"Does the Sveconorwegian ‘opx-in isograd’ exist?"}]},{"#name":"entry","$":{"id":"sec0155","depth":"3"},"$$":[{"#name":"label","_":"8.1.3"},{"#name":"title"," | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_486.txt | l-0.2-2.31c-0.89 0.79-2.94 1.55-4.69 1.55 -3.14 0-4.88-1.95-4.88-5.51v-0.49H48.06M39.91 9.18c0.17-0.17 1.29-0.46 1.98-0.46 2.48 0 3.76 0.53 3.86 3.43h-7.46C38.56 10.27 39. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_178.txt | window);
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_23.txt | and-Vest
Agder sectors. Internal divisions in the Rogaland-Vest
Agder sector, as proposed by Duchesne et al. (1999), are
not addressed in this paper. The Bamble-Kongsberg
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 89
Fig. 2. Geological sketchmap of SW Scandinavia showing th... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_4.txt | it
et al. (1998) and Nordgulen (1999). For one of the
sampling sites, namely Skånevik, an improved local
geological map is presented (See Fig. 5).
Zircon was separated for U-Pb geochronology using a
water table, heavy liquids and a magnetic separator.
Zircon from seven samples was analysed by isotope
dilution - thermal... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_57.txt | globalThis instanceof WorkerGlobalScope && globalThis.navigator instanceof WorkerNavigator),
o = n? window : "undefined"!= typeof WorkerGlobalScope && ("undefined"!= typeof self && self instanceof WorkerGlobalScope && self || "undefined"!= typeof globalThis && globalThis instanceof WorkerGlobalScope && glo... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_49.txt | as
the extrusion age of the rhyolite (Fig. 3). No evidence for
Sveconorwegian overprint is observed in the sample or
in the zircon data.
Sample FUN26 represents a little deformed granitic
gneiss (Fig. 2). The outcrop is made up of coarse-grained
granite characterized by centimetre-scale K-feldspar
megacrysts and by au... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_37.txt | al. 2002). Two main
types of metasedimentary complex are exposed. The
first type commonly shows a banding parallel to regional
structures and consists of metagreywacke-metapelite
associated with amphibolite and felsic orthogneisses
(Kongsberg complex, Selås Banded gneiss, Hisøy-Torungen complex; Starmer 1985; Knudsen ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_30.txt | H. & Whitehouse, M.J. 2003: Age and emplacement conditions of the Chalmers mafic intrusion deduced from
contact melts. GFF 125, 213-220.
Knudsen, T.-L., Andersen, T., Maijer, C. & Verschure, R.H. 1997a:
Trace-element characteristics and Pb isotopic evolution of metasediments and associated Proterozoic rocks from the am... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1399.txt | ]},{"#name":"entry","$":{"id":"sec0190","type":"appendices","depth":"1"},"$$":[{"#name":"label","_":"Appendix A"},{"#name":"title","$":{"id":"sect0210"},"_":"Supplementary data"}]},{"#name":"entry","$":{"id":"bibl0005","type":"bibliography","depth":"1"},"$$":[{"#name":"title","$":{"id":"sect0215"},"_":"References"}]}],... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_679.txt | 930 Ma. A metapelite in the immediate vicinity of the RAP yields a 950 Ma U–Pb age of matrix-hosted monazite, and part of the RAP was intruded by the Storgangen norite dike at ca. 950 Ma, providing a minimum age of emplacement. These ages are consistent with Ar–Ar hornblende and biotite ages that show r... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_623.txt | a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Earth Sci. Rev.</h3></div><div class="series">(2011)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>J. </span>Vander Auwera</span><em> et al.</em></span>... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_113.txt | class o {
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_39.txt | isotropic facies, Björshult Zrn 1368 ±4 Andersson et al., 1999
Torpa granite Zrn 1380 ±6 Åhäll et al., 1997
Tjärnesjö granite, veined facies, TJ25D Zrn 1394 ±11 Andersson et al., 1999
Stensjö granite pegmatite dyke, S4 Zrn 1399 +7/-6 Christoffel et al., 1999
Varberg charnockite-granite association, S8 Zrn 1399 +12 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1024.txt | -family":"serial","contentType":"JL","abstract":{"$$":[{"$$":[{"$":{"id":"sect0005"},"#name":"section-title","_":"Highlights"},{"$$":[{"$$":[{"$$":[{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0005"},"#name":"para","_":"We document the structural style in the basal shear zone of an eclogite-bearing napp... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_71.txt | 30 ±2 Heaman & Smalley, 1994
Telemark Morkheia monzonite suite, sheared monzonite M12 Zrn U-Pb 1132 ±3 Heaman & Smalley, 1994
Telemark Morkheia monzonite suite, monzonite M220 Zrn U-Pb 1134 ±2 Heaman & Smalley, 1994
Telemark Gunnarstul granite gneiss Zrn U-Pb 1134 ±21 Andersen et al., 2002
Telemark Heddal Gp, Skogs | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1386.txt | "},{"#name":"title","$":{"id":"sect0070"},"_":"Garnet granite"}]},{"#name":"entry","$":{"id":"sec0060","depth":"2"},"$$":[{"#name":"label","_":"4.5"},{"#name":"title","$":{"id":"sect0075"},"_":"Xenoliths and host rocks in and around the garnet granite"},{"#name":"entry","$":{"id":"sec0065","depth":"3"},"$$":[{"#name":"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_361.txt | r>svg{right:0}@media only screen and (max-width: 600px){#onetrust-pc-sdk.otPcCenter{left:0;min-width:100%;height:100%;top:0;border-radius:0}#onetrust-pc-sdk #ot-pc-content,#onetrust-pc-sdk.ot-ftr-stacked.ot-btn-container{margin:1px 3px 0 10px;padding-right:10px;width:calc( | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_27.txt | Hesjåbutind gabbro, central Telemark area,
Southern Norway. Geonytt 17, 38.
Dahlgren, S., Heaman, L. & Krogh, T. 1990b: Geological evolution and
U-Pb geochronology of the Proterozoic Central Telemark area,
Norway. Geonytt 17, 38-39.
Davis, W.J. & Peterson, T. 1998: New geochronological results for the
Tavani area (55K... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_15.txt | området Mineralogisk Geologisk Museum, 125, Oslo.
Berthelsen, A. 1980: Towards a palinspastic tectonic analysis of the
Baltic Shield. In Cogne, J. & Slansky, M. (eds.): Geology of Europe,
from Precambrian to the post-Hercyninan sedimentary basins, 108,
5-21. Mémoires du B.R.G.M., Paris.
Bingen, B. & van Breemen, O. 199... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_22.txt | -sdk li.ot-host-name a,#onetrust-pc-sdk li.accordion-text,#onetrust-pc-sdk li.ot-acc-txt{z-index:2;position:relative}#onetrust-pc-sdk input{margin:3px.1ex}#onetrust-pc-sdk.pc-logo,#onetrust-pc-sdk.ot-pc-logo{height:60px;width:180px;background-position:center;background- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_939.txt | si":true,"xmlns:cals":true,"xmlns:sb":true,"xmlns:sa":true,"xmlns:ja":true,"xmlns":true,"id":"sec0085","view":"all"},"$$":[{"#name":"label","_":"5"},{"#name":"section-title","$":{"id":"sect0100"},"_":"Host rock characteristics and relationships to the SMB"},{"#name":"para","$":{"id":"par0225","view":"all"},"_":"Identif... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_84.txt | var publishAge = Math.floor((nowTs - prodList[i].publishDate) / 86400);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1029.txt | a 4"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"km well-exposed section of the basal shear zone, we describe two major phases of deformation. An early deformation stage (D1) formed a penetrative gneissic foliation and tectonic layering, including isoclinal folds (F1). The sequence was subsequently aff... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_30.txt | terrane formed in a volcanic arc outboard of
the Palaeoproterozoic continent, possibly in front of a
back-arc basin (Åhäll et al. 1998; Brewer et al. 1998;
Bingen et al. 2001a; Bingen et al. 2004). The occurrence
of turbidite sequences with a narrow 1.66-1.53 Ga
provenance age restricted to the volcanic arc, is consis... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_881.txt | with intervening troughs of comparable length. Some magmatic peaks are observed on multiple cratons, either by coincidence or because of paleogeographic proximity and common tectonic setting, while others are not. The best overall correlation, 0.617, is observed between Baltica and Amazonia, consistent with (but not d... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_69.txt | .2716 2.23 0.99 1477 7 1549 31 104.9
13a 179 28 55 7943 0.09260 0.61 3.442 2.34 0.2696 2.26 0.97 1480 12 1539 31 104.0
09a 141 21 43 11064 0.09277 0.53 3.410 2.30 0.2666 2.24 0.97 1483 10 1524 30 102.7
08a 276 36 89 20333 0.09280 0.34 3.638 2.30 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_89.txt | Pb/206Pb 2 978 ±23 Bingen, unpublished
Rogaland-VA Augen gneiss, Feda, B135, TB Am 207Pb/206Pb 2 915.4 ±2.2 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Feda, B113, TC Am 207Pb/206Pb 3 915.6 ±1.8 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Feda, B120, | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_37.txt | : The age of the Hinneryd granite – its significance for
interpreting the terranes of the southern Baltic Shield. GFF 118,
163-168.
Lindh, A., Gorbatschev, R. & Lundegårdh, P.H. 1998: Beskrivning till
berggrundskartan över Värmlands Län; Västra Värmlands Berggrund. Sveriges Geologiska Undersökning Ser. Ba, 45:2, 1- | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_816.txt | postal-code","_":"NG12 5GG"},{"#name":"country","_":"UK"}]}]},{"#name":"affiliation","$":{"id":"aff0015"},"$$":[{"#name":"label","_":"c"},{"#name":"textfn","_":"Department of Geology and Mineral Resources Engineering, Norwegian University of Science and Technology, 7491 Trondheim, Norway"},{"#name":"affiliation","$":{"... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_9.txt | 0.90 1503 16 1760 27 117.1
1a 0.0938 0.0012 3.36 0.08 0.260 0.005 0.85 1505 23 1488 26 98.9
5c 0.0940 0.0009 3.62 0.07 0.279 0.005 0.87 1508 18 1588 24 105.3
5a 0.0940 0.0010 3.67 0.07 0.283 0.005 0.84 1509 20 1606 23 106.4
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