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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_50.txt | 95-112, Gol granite gneiss, Fig. E
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_659.txt | regime where partial melts drained into. Granitic gneisses react in a ductile manner and do not have the ability to drain partial melt.</p><p id="sp0020">Pegmatite formation in the Grenville Province, i.e., the Laurentian part of the Grenville–Sveconorwegian orogenic belt, formed between ca. 1090 and 980 Ma peaki... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_3.txt | Sveconorwegian orogenesis">
<meta property="og:title" content="The Late Mesoproterozoic Sirdal Magmatic Belt, SW Norway: Relationships between magmatism and metamorphism and implications for Sveconorwegian orogenesis">
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_717.txt | ="/science/article/pii/S0301926815001163" title="Hallandian 1.45Ga high-temperature metamorphism in Baltica: P–T evolution and SIMS U–Pb zircon ages of aluminous gneisses, SW Sweden"><span class="anchor-text"><span>Hallandian 1.45 Ga high-temperature metamorphism in Baltica: P–T evolution and SIMS U–Pb zircon ages... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_59.txt | , Earth
Science Centre, Göteborg University, Göteborg.
Berglund, J., Larson, S.Å. & Vinnefors, A. 1997: Sveconorwegian extension-parallel deformation structures; an example from the Hammarö Shear Zone, SW Sweden. GFF 119, 169-180.
Berthelsen, A. 1980: Towards a palinspastic tectonic analysis of the Baltic Shield. In Co... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen6.txt | part6 -------------------
Spatial heterogeneity[edit]
Additional studies have explored the spatial heterogeneity of kerogen at small length scales. Individual particles of kerogen arising from different inputs are identified and assigned as different macerals. This variation in starting material may lead to variations ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_667.txt | bsp;218.4°E, N = 38, A<sub>95</sub> = 6.1°, K = 15.6), central Telemark (P<sub>lat</sub> = -17.4° N, P<sub>long</sub> = 229.8° E, N = 23. A | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_17.txt | -Pb 1596 ±11 Larson et al., 1999
Tistedal granodiorite, Ø1 Zrn U-Pb 1599 +15/-16 Andersen et al., 2004
Göteborg suite, Åmal granodiorite Zrn U-Pb 1599 ±6 Åhäll & Connelly, 2008
Göteborg suite, Håle tonalite Zrn U-Pb 1602 ±10 Åhäll & Connelly, 2008
Lerum granite, 76263 Zrn U- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_487.txt | 71 9.37 39.91 9.18zM58.82 6.57c-2.24 0-3.63 1.12-4.85 2.61l-0.4-2.21h-2.34l0.13 1.19c0.1 0.76 0.13 1.78 0.13 2.97v10.79h2.54V11.88c0.69-0.96 2.15-2.48 2.48-2.64 0.23-0.13 1 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_23.txt | krift 64, 111-119.
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. 1999: Geochronology of the Rymmen gabbro, southern
Sweden; impli... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_50.txt | , A.G. 2007a: Timing and tectonic
significance of Sveconorwegian A-type granitic magmtism in Telemark, southern Norway: new results from laser-ablation ICPMS
U-Pb dating of zircon. Norges geologiske undersøkelse Bulletin 447,
17-31.
Andersen, T., Griffin, W.L. & Sylvester, A.G. 2007b: Sveconorwegian
crustal underplatin... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_937.txt | sect0035"},"_":"Field description and petrography of the Sirdal Magmatic Belt"},{"#name":"para","$":{"id":"par0080","view":"all"},"_":"In the following section we describe the different lithologies that constitute the SMB, and also the nature of xenoliths and host rocks found within and around the batholith. Determinat... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_59.txt | (%) (Ma) (Ma) (%) (1) (2) (2) (2) (3) (4) B98-43, Gøyst complex in Uvdal, metasandstone, Fig. 9A 20b 75 85 27 77700 0.09331 1.14 3.256 2.51 0.2531 2.24 0.89 1494 21 1454 29 97.3 15a 74 111 30 38625 0.09338 0.79 3.405 2.37 0.2644 2.24 0.94 14 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_491.txt | -6.01-7.56 -3.86 0-6.67 2.77-6.67 7.92 0 4.92 2.97 7.82 6.73 7.82 2.81 0 4.36-0.63 5.68-1.42l-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-0.49H92 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_65.txt | en lithosphere.
Indigenous Telemarkia
Most available geologic models picture the Sveconorwegian terranes as indigenous to Fennoscandia, either as
peripheral or as part of the margin of this craton during
the Mesoproterozoic (Fig. 9; Berthelsen 1980; Åhäll et al.
1998; de Haas et al. 1999; Åhäll & Larson 2000; Bingen et... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_2.txt | Ga). In that case,
the second Sveconorwegian suture would lie offshore to
the west or southwest of Rogaland.
Conclusions
Zircon U-Pb geochronological data presented in this
study demonstrate that the main continental building
event in the westernmost exposed domain in the Sveconorwegian orogen, namely the Telemark, Ha... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_52.txt | B., Birkeland, A. & Sigmond, E.M.O. 1997: Palaeo- to
Mesoproterozoic intrusive rocks in the area between Numedal and
Mjøsa, SE Norway. In Nordgulen, Ø., Padget, P., Robinson, P. &
McEnroe, S. (eds.), Copena Conference, 97.131, 69-70. Norges
geologiske undersøkelse, Trondheim.
Nordgulen, Ø. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_6.txt | bimodal magmatism and associated sediment basins in the Telemarkia
Terrane. At 1140 Ma, collision between the Telemarkia
and Idefjorden Terranes produced an orogenic wedge
consisting of the Bamble and Kongsberg Terranes. This
process resulted in crustal thickening with metamorphism peaking in intermediate-pressure gra... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_839.txt | within the Sveconorwegian orogeny is discussed."}],"$":{"id":"o0010"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0015"},"#name":"para","_":"We report new ∼ 1090 Ma, ∼1000 Ma, and ∼ 900 Ma paleomagnetic poles for Baltica."}],"$":{"id":"o0015"},"#name":"list-item"},{"$$":[{"#name":"l... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_93.txt | orden norite, contact melt HAS96003 Zrn U-Pb 916 ±11 Scherstén et al., 2000
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_14.txt | .223 0.004 0.85 1506 20 1299 20 86.3
5 0.0940 0.0011 3.01 0.05 0.232 0.003 0.77 1508 22 1345 17 89.2
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 111
Atomic ratios Ages
Sample/ 207Pb ±σ 207Pb ±σ 206Pb ±σ rho 207Pb ±σ 206Pb ±σ Disc.
analysis 206Pb | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_72.txt | åa porphyry, TA992 Zrn U-Pb 1145 ±4 Laajoki et al., 2002
Telemark Eiddal granite gneiss, N95-65 Zrn U-Pb 1146 ±5 Bingen et al., 2003
Telemark Hesjåbutind gabbro sill Zrn U-Pb 1146 ±2 Dahlgren et al., 1990
Telemark Høydalsmo Gp, Dalaå porphyry, 830KLN Zrn U-Pb 1150 ±4 Laajoki | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_36.txt | ;
Andersen & Laajoki 2003; Andersen et al. 2004b; Laajoki & Corfu 2007). The lower sequence is made up of
the 1510-1500 Ma bimodal volcanic rocks of the Rjukan
Group. It is overlain by the quartzite-dominated Vindeggen Group. The overlying unconformable sequence is
made up of 1170-1140 Ma bimodal volcanic rocks interla... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_540.txt | 0f544990f7288c6b5a2362d06486df/image/elsevier-non-solus.png" alt="Elsevier"></span></a></div><div class="publication-volume u-text-center"><h2 class="publication-title u-h3" id="publication-title"><a class="anchor publication-title-link anchor-navigation" href="/journal/precambrian-research" title="Go to Precambrian Re... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_77.txt | 3.5080 1.47 0.27003 1.41 0.96 1513 8 1541 19 101.9
B02-027, Botsvatn gneiss complex, granite gneiss, Fig. 9D
03a (5) 158 45 49 18549 0.09094 0.58 3.2866 1.52 0.26213 1.41 0.92 1445 11 1501 19 103.8
19a 135 40 41 10865 0.09191 0.81 3.2972 1.63 0.26 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_962.txt | , East Perth, WA 6004, Australia"},{"#name":"affiliation","$":{"xmlns:sa":true},"$$":[{"#name":"organization","_":"Geological Survey of Western Australia"},{"#name":"address-line","_":"100 Plain St"},{"#name":"city","_":"East Perth"},{"#name":"state","_":"WA"},{"#name":"postal-code","_":"6004"},{"#name":"country","_":"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_615.txt | series"><h3 class="title">Precambrian Res.</h3></div><div class="series">(2008)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>C.M. </span>Mottram</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1048.txt | osciences"},{"#name":"address-line","_":"Xueyuan Road 29#"},{"#name":"address-line","_":"Haidian District"},{"#name":"city","_":"Beijing"},{"#name":"postal-code","_":"100083"},{"#name":"country","_":"China"}]}]},{"#name":"affiliation","$":{"id":"af015"},"$$":[{"#name":"label","_":"c"},{"#name":"textfn","_":"Institute o... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1031.txt | assemblages. D2 shear structures are associated with top-to-the-east kinematic indicators throughout the section. The D1 episode was responsible for emplacement of the eclogite-nappe into its present structural position. The subsequently developed lineation-parallel folds are interpreted to form by general shear, wher... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_14.txt | i = r(3117);
const o = "nr@original:".concat(i.a);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_87.txt | onetrust-pc-sdk ul ul,#ot-sdk-cookie-policy ul ul{margin:1.5rem 0 1.5rem 3rem;font-size:90%}#onetrust-banner-sdk li,#onetrust-pc-sdk li,#ot-sdk-cookie-policy li{margin-bottom:1rem}#onetrust-banner-sdk th,#onetrust-banner-sdk td,#onetrust-pc-sdk th,#onetrust-pc- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1068.txt | -MgO-Al"},{"$":{"loc":"post"},"#name":"inf","_":"2"},{"#name":"__text__","_":"O"},{"$":{"loc":"post"},"#name":"inf","_":"3"},{"#name":"__text__","_":"-SiO"},{"$":{"loc":"post"},"#name":"inf","_":"2"},{"#name":"__text__","_":"-H"},{"$":{"loc":"post"},"#name":"inf","_":"2"},{"#name":"__text__","_":"O-TiO"},{"$":{"loc | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_71.txt | aton (Baltica)
before and during the assembly of Rodinia. Precambrian Research
160, 23-45.
Bolle, O., Diot, H. & Duchesne, J. C. 2000: Magnetic fabric and deformation in charnockitic igneous rocks of the Bjerkreim-Sokndal
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1110.txt | ","$":{"id":"aut0045"},"$$":[{"#name":"given-name","_":"Michel"},{"#name":"surname","_":"Bogaerts"},{"#name":"cross-ref","$":{"id":"crf0885","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]},{"#name":"affiliation","$":{"id":"aff0005"},"$$":[{"#name":"label","_":"a"},{"#name":"textfn","_":"Departme... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1392.txt | _":"6.2.2"},{"#name":"title","$":{"id":"sect0135"},"_":"MM02277"}]}]},{"#name":"entry","$":{"id":"sec0125","depth":"2"},"$$":[{"#name":"label","_":"6.3"},{"#name":"title","$":{"id":"sect0140"},"_":"Xenoliths and host rocks to the SMB"},{"#name":"entry","$":{"id":"sec0130","depth":"3"},"$$":[{"#name":"label","_":"6.3.1"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_349.txt | cntr ul.ot-subgrps.ot-acc-hdr.ot-chkbox label::before,#onetrust-pc-sdk.ot-vs-list.ot-vnd-item.ot-acc-hdr.ot-chkbox label::before,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-item.ot-acc-hdr.ot-chkbox label::before,#onetrust-pc-sdk #ot-pc-lst. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_179.txt | ||[],window.ddqueue.push(dispatcherData),window.eventData=dispatcherData.eventData,window.pageData=dispatcherData.pageData,_satellite.track(dispatcherData.eventName)}catch(e){_satellite.logger.log("eventDispatcher: exception"),_satellite.logger.log(e)}
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_60.txt | r.d(t, {
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_725.txt | =recommended-articles:type=close"><span class="button-link-text"><h2 class="section-title u-h4"><span class="related-content-panel-title-text">Recommended articles</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 4... | |
no_hydrocarbons_in_sveconorwegian_belt/Kerogen7.txt | part7 -------------------
Types[edit]
Labile kerogen breaks down to generate principally liquid hydrocarbons (i.e., oil), refractory kerogen breaks down to generate principally gaseous hydrocarbons, and inert kerogen generates no hydrocarbons but forms graphite.
In organic petrography, the different components of kerog... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_reservoir1.txt | part1 -------------------
A petroleum reservoir or oil and gas reservoir is a subsurface accumulation of hydrocarbons contained in porous or fractured rock formations. Such reservoirs form when kerogen (ancient plant matter) is created in surrounding rock by the presence of high heat and pressure in the Earth's crust.
... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_trap4.txt | part4 -------------------
Hybrid trap[edit]
Hybrid trap formed by the mudstone draping of tilted blocks
Hybrid traps are the combination of two types of traps. In the case of tilted blocks, the initial reservoir geometry is the one of a fault-controlled structural trap, but the caprock is generally made by the draping ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_48.txt | and compositions of the high-grade metamorphic Nidelva Quartzite Complex (Bamble, Norway), and the
origin of nodular gneisses. Proceedings Koninklijke Nederlandse
Akademie van Wetenschappen 96, 217-232.
Nordgulen, Ø. 1999: Geologisk kart over Norge, berggrunnskart
Hamar, 1:250000. Norges geologiske undersøkelse.
O’Nio... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_14.txt | the error on the
day-to-day calibration curve obtained by regular
analysis of the reference zircon. A common Pb
correction is applied using the 204Pb analysis.
The LA-ICPMS data were collected on a Finnigan
ELEMENT1 single collector high-resolution sector
ICPMS, alimented by a Finnigan 266 nm laser
microsampler. The a... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_0.txt | 11 0.0934 0.0011 2.97 0.06 0.230 0.004 0.81 1497 23 1335 20 89.2
1 0.0938 0.0009 3.17 0.06 0.245 0.004 0.85 1505 19 1412 20 93.8
17a 0.0940 0.0009 3.28 0.07 0.253 0.005 0.88 1509 19 1454 23 96.3
4 0.0942 0.0013 3.32 0.07 0. | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_103.txt | t.aborted || (n.duration = (0, g.z)() - this.startTime, this.loadCaptureCalled || 4!== e.readyState? null == t.status && (t.status = 0) : _(this, e), n.cbTime = this.cbTime, i("xhr", [t, n, this.startTime, this.endTime, "xhr"], this, r.D.ajax));
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_420.txt | #ot-pc-desc{padding:0}div#onetrust-pc-sdk #ot-pc-desc a{display:inline}div#onetrust-pc-sdk #accept-recommended-btn-handler{display:none!important}div#onetrust-pc-sdk input[type=checkbox]:focus+.ot-acc-hdr{outline:2px solid #eb6500;outline-offset:-1px;transition:none}div#onetrust-pc-sdk.ot-accord | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_73.txt | et al., 2002
Telemark Fjellstadfjell granite, 072696-1 Zrn U-Pb 1151 ±9 Andersen et al., 2007
Telemark Haglebu granite gneiss, N95-113 Zrn U-Pb 1153 ±2 Bingen et al., 2003
Telemark Brunkeberg Fm, porphyry, 903KLN Zrn U-Pb 1155 ±2 Laajoki et al., 2002
Telemark Oftefjell Gp, Ljosdalsvat | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_447.txt | sdk-cookie-policy-group-desc,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy.ot-table-header,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy a,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy span,#ot-sdk-cookie-policy-v2.ot-sdk-cookie-policy td{font-size:.9em}#ot-sd | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1090.txt | and bimodal volcanism at the onset of the Sveconorwegian Orogeny, southern Norway"}],"floats":[],"footnotes":[],"attachments":[]},"openArchive":false,"openAccess":false,"document-subtype":"fla","content-family":"serial","contentType":"JL","abstract":{"$$":[{"$$":[{"$":{"id":"sect0005"},"#name":"section-title","_":"Hig... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_756.txt | ><li><a class="anchor u-display-block u-clr-grey8 u-margin-s-bottom u-margin-0-bottom-from-sm u-margin-m-right-from-sm u-margin-l-right-from-md anchor-default" href="http://elsmediakits.com" target="_blank" id="els-footer-advertise" rel="nofollow"><span class="anchor-text">Advertise</span><svg focusable="false" viewBox... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1471.txt | ,10.566,25.837l186.146,185.864c7.05,7.043,15.66,10.564,25.841,10.564
s18.795-3.521,25.834-10.564l21.409-21.412c7.05-7.039,10.567-15.604,10.567-25.697c | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_621.txt | ="_self"><span class="anchor-text">Left-lateral transpressive deformation and its tectonic implications, Sveconorwegian orogen, Baltic Shield, southwestern Sweden</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Precambrian Res.</h3></div><div class="series">(1996)</div></... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_25.txt | Vest Agder sector, displays
a SE-NW to N-S structural pattern. It consists of felsic
orthogneisses and subordinate volumes of anatectic
garnet-bearing gneiss, quartzite and mafic gneiss
(Falkum 1985; Tobi et al. 1985). Few pre-Sveconorwegian U-Pb dates are recorded (Table 10).
Available data include a poorly defined up... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_52.txt | new I("string" == typeof e? e : (0, D.P)(e));
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1339.txt | ","_":"B.W.H."},{"#name":"surname","_":"Hendriks"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"The Grenvillian-Sveconorwegian orogeny in Fennoscandia: back-thrusting and extensional shearing along the Mylonite Zone"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$"... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_41.txt | t.emit(i + "before-start", [r], a), a[n.A] && a[n.A].dt && (e = a[n.A].dt);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_938.txt | in Electronic Supplement 2."},{"#name":"para","$":{"id":"par0085","view":"all"},"_":"The geographic extent of the SMB, as shown in Fig. 1a, is based on mapping by the Geological Survey "}]}]},{"#name":"section","$$":[{"#name":"section","$":{"xmlns:ce":true,"xmlns:mml":true,"xmlns:xs":true,"xmlns:xlink":true,"xmlns:xoc... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_35.txt | video.id, data.video.position);
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