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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_957.txt | .1016/j.precamres.2014.12.001","journalTitle":"Precambrian Research","publicationYear":"2015","publicationDate":"2015-08-01","volumeSupText":"Volume 265","articleNumber":"","pageRange":"218-231","trace-token":"AAAAQBmEilysDXkD7OK1VKES7UWiA9gDew_6uZ2wtPLYIO0JvvxWjVAVBK2hk6er069mcMGx4LBLTd0DMP | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_932.txt | a","$":{"id":"par0035","view":"all"},"$$":[{"#name":"__text__","_":"The study area is located in the southwesternmost part of the Sveconorwegian Province and has previously been interpreted to consist of high-grade ortho- and lesser amounts of para- and banded gneisses that were deformed and metamorphosed between ca. 1... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_505.txt | Books"><span class="anchor-text">Journals & Books</span></a></li></ul></nav><nav aria-label="utilities" class="gh-nav gh-nav-utilities gh-nav-h"><ul class="gh-nav-list u-list-reset"><li class="gh-move-to-spine gh-help-button gh-help-icon gh-nav-item"><div class="popover" id="gh-help-icon-popover"><div id="popover-... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_678.txt | that the RAP is located in the footwall of a 15 km-wide extensional detachment (Rogaland Extensional Detachment, RED), separating the intrusions and their UHT host rocks from weakly metamorphosed rocks in the hanging wall. U–Pb zircon dating of leucosome in extensional pull-aparts associated with the RED yields a... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_16.txt | häll, 1996
Red syeno-granite gneiss, Lake Racken, DC972 Zrn U-Pb 1590 ±14 Larson et al., 1999
Töcksfors granodiorite Zrn U-Pb 1594 ±7 Åhäll & Connelly, 2008
Harnäs gneiss, Hn96093 Zrn U-Pb 1595 +24/-17 Alm et al., 2002
Grey quartz monzodiorite gneiss, Lake Racken, DC9413 Zrn U | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_97.txt | ble Marble, Tromøy, 92-10, Sph9210a Gr 207Pb/206Pb 1 1137 ±2 Cosca et al., 1998
Idefjorden Terrane
Veddige augen gneiss, Mylonite Zone Am 207Pb/206Pb 5 953 ±6 Andersson, 2001
Migmatitic granitoid, Fölsbyn, SWS-38 Am 207Pb/206Pb 1 1023 c. Connelly & Åhäll, 1996
Begna Migmatitic | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_221.txt | -subhdr{width:100%;display:inline-block}#onetrust-pc-sdk.ot-search-cntr{float:left;width:78%;position:relative}#onetrust-pc-sdk.ot-search-cntr>svg{width:30px;height:30px;position:absolute;float:left;right:-15px}#onetrust-pc-sdk.ot-fltr-cntr{float:right;right:50px;position:relative}#onet | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_7.txt | 0000. Norges geologiske undersøkelse Bulletin 341,
1-94.
Sigmond, E.M.O., Gjelle, S. & Solli, A. 1997: The Rjukan Proterozoic
rift basin, its basement and cover, volcanic and sedimentary infill,
and associated intrusions. Norges geologiske undersøkelse Bulletin
433, 6-7.
Sigmond, E.M.O. 1998: Geologisk kart over Norge,... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_160.txt | - Online State'
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1289.txt | ","$$":[{"#name":"maintitle","_":"Zircon Lu–Hf isotopes in high-alumina orthopyroxene megacrysts from the Neoproterozoic Rogaland Anorthosite Province, SW Norway: a window into the Sveconorwegian lower crust"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"main... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_28.txt | to amphibolite-facies tholeiitic to calcalkaline magmatic suites and metagreywacke sequences
(Åhäll et al. 1998; Brewer et al. 1998; Åhäll et al. 2000).
Metavolcanic rocks include the 1643 ± 29 Ma Horred
formation, 1614 ± 7 Ma Åmål formation, and 1615 ±
31 Ma Slemmestad metarhyolite (Table 8; Lundqvist &
Skiöld 1993; ... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_73.txt | al, 92-12c U-Pb ID-TIMS 1 Cosca et al., 1998
NORWEGIAN JOURNAL OF GEOLOGY A four-phase model for the Sveconorwegian orogeny, SW Scandinavia 55 Idefjorden Terrane Zrn 917±13 Am Migmatitic granodiorite, Stora Lundby, leucosome 9701a U-Pb SIMS 12 Scherstén et al., 2004 Zrn 971±8 Am Red syeno-granite gneiss, Lake | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_927.txt | conorwegian Province may not be a direct continuation of the Grenville Province. The Sveconorwegian orogeny in S Norway and SW Sweden involved magmatic, metamorphic and deformational processes of variable character that took place across different parts of the orogen at different times between ca. 1200 and 900"},{"#nam... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_438.txt | onetrust-pc-sdk #clear-filters-handler,div#onetrust-pc-sdk button#filter-apply-handler,div#onetrust-pc-sdk button#filter-cancel-handler{height:2em!important;padding-left:14px!important;padding-right:14px!important}div#onetrust-pc-sdk #ot-fltr-cnt{box-shadow:0 0;border:1px solid #8e8e8e;border-radius:0}div | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_157.txt | -hdr{outline:2px solid #eb6500;outline-offset:-1px;transition:none}div#onetrust-pc-sdk.ot-accordion-layout.ot-cat-item{border-width:0 0 2px}div#onetrust-pc-sdk.ot-accordion-layout.ot-cat-item:first-of-type{border-width:2px 0}div#onetrust-pc-sdk.ot-accordion-layout.ot-acc | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_656.txt | veconorwegian orogeny rather than to be highly evolved residual melts derived from granites. We test this hypothesis by providing new age data for thirteen pegmatites and one granite. Based on these new age data, we distinguish two age groups of Sveconorwegian pegmatites (>1,000 m<sup>3</sup> in size); Group 1:... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_18.txt | Kullerud & Dahlgren 1993). Several isograds show
that the regional metamorphic grade increases across
strike to the southeast and reaches intermediate-pressure
granulite-facies conditions in the Arendal area (Touret
1971; Smalley et al. 1983; Nijland & Maijer 1993). Peak
pressure-temperature conditions are estimated t... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_6.txt | age of
two orthogneisses in the Proterozoic Mjøsa-Vänern ore district,
southwestern Scandinavia. GFF 124, 45-61.
Andersen, T. 1997: Radiogenic isotope systematics of the Herefoss
granite, South Norway: an indicator of Sveconorwegian
(Grenvillian) crustal evolution in the Baltic shield. Chemical Geology
135, 139-158.
A... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_90.txt | }
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_60.txt | presence of an oceanic basin at the onset of the
Sveconorwegian orogeny. Location of the Tromøy complex in the small Bamble Terrane is compatible with closure of the basin between the Idefjorden and Telemarkia
Terranes (Fig. 7; Fig. 9). (2) In the Telemarkia and Bamble Terranes, widespread continental bimodal magmatis... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1093.txt | ":"par0020"},"#name":"para","_":"The basalts have compositions akin to melting of an enriched asthenospheric wedge."}],"$":{"id":"lsti0020"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0025"},"#name":"para","_":"The sedimentary rocks record alternating multi- and unimodal zircon ag... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_22.txt | mafic layers of possible volcanic origin. Felsic layers commonly
contain cm-scale K-feldspar megacrysts, clearly linking them to a
plutonic or sub-volcanic protolith. Sample B02027, is collected from
the ca. 1.5 m thick layer of granite gneiss with a linear augen texture
in the centre of the photo (collected in front ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_636.txt | continental building in the Sveconorwegian orogen, SW Scandinavia</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Nor. J. Geol.</h3></div><div class="series">(2005)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-san... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1240.txt | Precambrian Res."}]},{"#name":"volume-nr","_":"160"}]},{"#name":"date","_":"2008"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"179"},{"#name":"last-page","_":"210"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0175"},"$$":[{"#name":"label","_":"Möller et al., 2002"},{"#name":"reference","$":{"id":"sbref0175",... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_43.txt | R.A. 1999: Emplacement
ages and metamorphic overprinting of granitoids in the Sveconorwegian Province in Värmland, Sweden - an ion probe study. Norsk
Geologisk Tidsskrift 79, 87-96.
Lindh, A., Schöberg, H. & Annertz, K. 1994: Disturbed radiometric
ages and their bearing on interregional correlations in the SW
Baltic S... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_16.txt | ectonic regimes and terrane
boundaries in the high-grade Sveconorwegian belt of SW Norway,
inferred from U-Pb zircon geochronology and geochemical
signature of augen gneiss suites. Journal of the Geological Society,
London 155, 143-154.
Bingen, B. & van Breemen, O. 1998b: U-Pb monazite ages in amphibolite- to granulite... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1407.txt | ":"product:journal:article","noTracking":"false","productAppVersion":"abstract-direct","productName":"SD","type":"CP-CA","environment":"prod","loadTimestamp":1711418024558,"loadTime":""},"visitor":{"accessType":"ae:ANON_GUEST","accountId":"ae:228598","accountName":"ae:ScienceDirect Guests","loginStatus":"anonymous","us... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_880.txt | which all cratons studied were involved in the Rodinia-forming Grenvillian orogeny. However, the magmatic record is not smooth and even but highly irregular, with marked peaks and troughs, both for individual cratons and the combined data set."}],"$":{"view":"all","id":"sp0015"},"#name":"simple-para"},{"$":{"view":"al... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1316.txt | #name":"surname","_":"Ellis"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"In situ U–Pb dating of zircon formed from retrograde garnet breakdown during decompression in Rogaland, SW Norway"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_8.txt | .0 GPa-700
°C. This metamorphism lies between 1046 ±6 and 1026
±5 Ma according to zircon U-Pb data and Sm-Nd and
Lu-Hf mineral isochrons (Table 4; Söderlund et al. 2008).
Amphibolite-facies metamorphism, west of the Göta Älv
Shear Zone and Dalsland Boundary Zone lies between
1043 ±11 Ma and c. 1023 Ma according to zirc... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_847.txt | name":"inf","_":"95"},{"#name":"__text__","_":" = 12.0, K = 19.4) were assigned 1090 Ma, 1000 Ma, and 900 Ma ages, respectively. The new Bamble paleomagnetic pole reconstructs Baltica at ∼ 1090 Ma with noticeable latitudinal gap from the eastern Laurentian margin and thus does not support classical Baltica-Laurentia co... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1178.txt | ","_":"M.N."},{"#name":"surname","_":"Ducea"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M.D."},{"#name":"surname","_":"Barton"}]}]},{"#name":"title","$$":[{"#name":"maintitle","_":"Igniting flare-up events in Cordilleran arcs"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name"... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_20.txt | Bingen et al. 2008b)
and by titanite in marble at 1137 ±2 Ma (Fig. 4; Cosca
et al. 1998). A monazite at 1137 ±1 Ma in a sillimanitebearing granulite probably dates peak granulite-facies
conditions (Hisøy locality; Bingen et al. 2008b).
The second metamorphic phase covers both the Bamble
and Kongsberg Terranes. In the ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_60.txt | h2,#onetrust-banner-sdk h3,#onetrust-banner-sdk h4,#onetrust-banner-sdk h5,#onetrust-banner-sdk h6,#onetrust-pc-sdk h1,#onetrust-pc-sdk h2,#onetrust-pc-sdk h3,#onetrust-pc-sdk h4,#onetrust-pc-sdk h5,#onetrust-pc-sdk h6,#ot- | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_166.txt | %; width: auto; text-align: center; border: 3px outset; padding: 1em 2em; background-color: #DDDDDD; color: black; cursor: default; font-family: message-box; font-size: 120%; font-style: normal; text-indent: 0; text-transform: none; line-height: normal; letter-spacing: normal; word-spacing: normal; word-wrap: normal; w... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1287.txt | first-page","_":"173"},{"#name":"last-page","_":"181"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0250"},"$$":[{"#name":"label","_":"Sauer et al., 2013"},{"#name":"reference","$":{"id":"sbref0250","refId":"50"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_120.txt | ,prodList[i].id // id
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_19.txt | with the westwards increase in volume of syn-collisional
magmatism, this contrast reflects the warmer thermal
nature of the crust in the Telemarkia Terrane relative to
the Idefjorden Terrane.
Falkenberg phase, 980-970 Ma
At 980-970 Ma (Fig. 8d), high-grade metamorphism is
recorded in the Eastern Segment, implying that ... | |
no_hydrocarbons_in_sveconorwegian_belt/Petroleum_trap5_0.txt | part5 -------------------
See also[edit]
Petroleum reservoir
Structural geology
| |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_897.txt | .0-S0024493721003030-main.pdf"}},{"articleTitle":"Tracing the Sveconorwegian orogen into the Caledonides of West Norway: Geochronological and isotopic studies on magmatism and migmatization","authors":"Wang C.-C., Wiest J.D., Jacobs J., Bingen B., Whitehouse M.J., Elburg M.A., Sørstrand T.S., Mikkelsen L., Hestnes Å.",... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_64.txt | neiss, Liland, B107 U-Pb ID-TIMS 2 Bingen & van Breemen, 1998
Rogaland-VA Zrn 1015 ±11, 964±3, 928±10, 909±13 Gr Migmatitic aluminous granulite, Gyadalen, 12E U-Pb SIMS 30 Möller et al., 2002
Rogaland-VA Zrn 1017±6 to 970±6, 922±14 Gr Charnockitic gneiss, Gyadalen, 19A | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_106.txt | FN_END: () => c,
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_0.txt | of magmatic and sedimentary rocks exposed in the Idefjorden and Telemarkia Terranes can be derived by various combinations of crustal reservoirs exposed in the
western part of Fennoscandia and of mantle reservoirs
(Andersen et al. 2001; Andersen et al. 2002b; Andersen &
Laajoki 2003). (3) Quartzite dominated clastic se... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_38.txt | Suldal Suldal supra granodiorite gneiss strong B00-140 357548 6597318 Bt, Amp, Ep, Ttn LA-ICPMS 11 10 0.71 1519 12 intrusion 10D
Metasediment
Telemark sector
Uvdal Gøyst metasandstone medium B98-43 483400 6679600 Bt, Ms, Grt SIMS 21 8 0.91 1508 10 detrital 9A
2 1635 23 detrital
3 1751 30 detrit | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_877.txt | Rodinia."}],"$":{"id":"o0030"},"#name":"list-item"}],"$":{"id":"l0005"},"#name":"list"}],"$":{"view":"all","id":"sp0010"},"#name":"simple-para"}],"$":{"view":"all","id":"as010"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab010","lang":"en","class":"author-highlights"},"#name":"abstract"},{"$$":[{"$":{"id":"st015... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_703.txt | 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="sp0010">The Sveconorwegian orogen represents a branch of Grenville-age (~1250–950 Ma) orogenic belt... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1450.txt | 446 2.709-1.251 5.01-2.59 6.906-4.016zm5.87 13.88a.75.75 0 00-.974.159l-5.475 6.625-3.005-2.997-.077-.067a.75.75 0 00-.983 1.13l4.172 4.16 6.525-7.895.06-.083a.75.75 0 00-.16-.973z" fill="#FFF" fill-rule=" | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_58.txt | -TIMS 4 Bingen & van Breemen, 1998
Rogaland-VA Mnz 1002±7 Am Granitic gneiss, Knaben II mine, B0128 U-Pb SIMS 11 Bingen et al., 2008
Rogaland-VA Mnz 927±5, 924±5 Am Augen gneiss, Sirdal, B185 Th-Pb ID-TIMS 2 Bingen et al., 2008
Rogaland-VA Mnz 1006±3, 975±2, 912 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_27.txt | . 1996).
Discussion
Timing of continental building
Figure 7 and Tables 1, 7-10 summarize available U-Pb
dates on magmatic events in the Sveconorwegian orogen.
The oldest cluster of peaks in the relative probability
curve defines the main period of continental building
in each domain (Fig. 7).
In the Eastern Segment, co... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_94.txt | , B99114 Am 207Pb/206Pb 3 985 ±5 Bingen et al., 2008
Rogaland-VA Augen gneiss, Liland, B107, TA Gr 207Pb/206Pb 1 919 ±6 Bingen & van Breemen, 1998
Rogaland-VA Augen gneiss, Sira, B198, TA Gr 207Pb/206Pb 2 919.8 ±4.2 Bingen & van Breemen, 1998
Bamble and Kongsberg Terranes
Bam | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_40.txt | ell and Saggrenda-Sokna shear zones and to the
north-west of the Kristiansand-Porsgrunn shear zone
(Figs. 1, 2). It consists of a large, greenschist- to epidoteamphibolite-facies supracrustal sequence with a total
thickness exceeding 10 km, surrounded by amphibolitefacies gneiss complexes. In the low-grade region of
ce... | |
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