id stringlengths 15 145 | text stringlengths 2 241k | title stringclasses 1
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_74.txt | net porphyry, 902KLN Zrn U-Pb 1155 ±3 Laajoki et al., 2002
Telemark Venås quartz monzonite-granite, 071996-1 Zrn U-Pb 1157 ±7 Andersen et al., 2007
Rogaland Hidderskog charnockite gneiss Zrn U-Pb 1159 ±5 Zhou et al., 1995
Telemark Sørkjevatn Fm, metarhyolite-microgranite, B9825 Zrn U | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_7.txt |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_704.txt | continent Rodinia. This study traces the Sveconorwegian records from its type-area in the Baltic Shield of South Norway into basement windows underneath Caledonian nappes, by combining zircon U–Pb geochronology and Hf–O isotopes. Samples along a N-S trending transect reveal multiple magmatic episodes during Gothian (ca... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_889.txt | belonging to the high-grade gneiss complex characteristic of the wall rocks of the Rogaland anorthosite province. Instead they have strong similarities with a high-alumina basalt that is the possible parental magma of the EGOG anorthosite. Slight variations from norite to leuconorite compositions were induced by metam... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing1_11.txt | Marker, E. M. O. Sigmond, Ø. Nordgulen, Geological Survey of Norway, NO-7491 Trondheim Norway (e-mail:
bernard.bingen@ngu.no); J. Ragnhildstveit, Hordaland County Council, PO Box 7900, NO-5020 Bergen, Norway; J. Mansfeld, Department of Geology
and Geochemistry, Stockholm University, SE-10691 Stockholm, Sweden; R. D. T... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1131.txt | itle","_":"Incremental pluton emplacement by magmatic crack-seal"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Trans. R. Soc. Edinb.: Earth Sci."}]},{"#name":"volume-nr","_":"97"}]},{"#name":"date","_":"2006"}]},{"#name":"pages","$$":[{"#name... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_19.txt | Wahlgren, C.-H., Cruden, A.R. & Stephens, M.B. 1994: Kinematics of a
major fan-like structure in the eastern part of the Sveconorwegian
orogen, Baltic Shield, south-central Sweden. Precambrian Research
70, 67-91.
Wahlgren, C.-H., Heaman, L.M., Kamo, S. & Ingvald, E. 1996: U-Pb
baddeleyite dating of dolerite dykes in th... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_894.txt | •"},{"$":{"view":"all","id":"p0015"},"#name":"para","_":"Felsic anatectic melts are produced by disequilibrium melting of the country rocks."}],"$":{"id":"li0015"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0020"},"#name":"para","_":"The parent magma and the felsic material did not ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1233.txt | Igneous Rocks and Glossary of Terms: Recommendations of the International Union of Geological Sciences Subcommission on the Systematics of Igneous Rocks"}]}]},{"#name":"host","$$":[{"#name":"book","$$":[{"#name":"date","_":"1989"},{"#name":"publisher","$$":[{"#name":"name","_":"Blackwell Scientific Publications"},{"#n... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_38.txt | (Hallingdal Complex; Fig. 4). Metamorphism
is dated at 1014 ±1 Ma by means of zircon in an amphibolite boudin (Bingen et al. 2008b). This is consistent with
the observation that the Heddal group (<1121 ±15 Ma)
is overprinted by this metamorphism. Towards the south,
supracrustal rocks abut a NE-SW trending amphibolitef... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing3_54.txt | Baadsgaard, H. 1971: A radiometric study of
polymetamorphism in the Bamble region, Norway. Contributions
to Mineralogy and Petrology 34, 1-21.
Park, R.G., Åhäll, K.-I. & Boland, M.P. 1991: The Sveconorwegian
shear-zone network of SW Sweden in relation to mid-Proterozoic
plate movements. Precambrian Research 49, 245-26... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_35.txt | 1080 Ma, the early-Sveconorwegian Arendal
phase is interpreted as an early collision of comparatively
restricted extent. Collision between the Idefjorden and
Telemarkia Terranes generated the Bamble and Kongsberg orogenic wedges, possibly as a result of accretion of
the Telemarkia Terrane. (2) At 1050-980 Ma, the Agder... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_42.txt | .7
(1) Analysis identifier, p: first surface ablation, x: not used for age calculation (2) Measured ratio (3) Ratio corrected for common Pb
(4) Correlation of errors (5) Age corrected for common Pb (6) Discordance of the analysis: 100-(100 x (206Pb/238U)age / (207Pb/206Pb)age)
Table 1. LA-ICPMS U-Pb data on zircon from... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_42.txt | 235
U 238
U 206Pb
(µg) (ppm) (ppm) (pg) (Ma) (%)
(1) (2) (2) (2) (3) (4) (5) (6) (6) (6) (7) (8)
N95-95, Vindflomyra granodioritic gneiss, Fig. 8A
1 3gr,+75,pb,t-pr 11 36.1 117 1 0.57 15313 0.09908 5 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1091.txt | par0005"},"#name":"para","_":"We report zircon U-Pb/Hf/O isotopes from the Bandak succession in Telemark, Norway."}],"$":{"id":"lsti0005"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"par0010"},"#name":"para","_":"These rocks record 3 phases of sedimentation and eruption of bimodal vol... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_114.txt | osome dates one of the WNWESE trending folds at 976 ±7 Ma (Oxanäset locality; Fig.
4; Möller et al. 2007), i.e. this fold is coeval, within error,
with the age of eclogite-facies metamorphism. Cross-cutting granitic dykes place the end of ductile deformation
at 956 ±7 Ma in one of the high-strain zones (Möller &
Söderl... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_78.txt | 018 1.41 0.87 1466 15 1491 19 101.7
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1322.txt | era et al., 2003"},{"#name":"reference","$":{"id":"sbref0315","refId":"63"},"$$":[{"#name":"contribution","$":{"langtype":"en"},"$$":[{"#name":"authors","$$":[{"#name":"author","$$":[{"#name":"given-name","_":"J."},{"#name":"surname","_":"Vander Auwera"}]},{"#name":"author","$$":[{"#name":"given-name","_":"M."},{"#name... | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_21.txt | 3 0.0948 0.0007 3.18 0.04 0.243 0.003 0.85 1524 13 1403 14 92.1
13 0.0953 0.0013 3.38 0.09 0.257 0.006 0.87 1535 25 1473 32 96.0
10 0.0969 0.0012 3.32 0.05 0.249 0.003 0.69 1565 22 1432 14 91.5
B00-149, granite gneiss, Vanvik, Fig. 10H
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_82.txt | ±3 Bingen et al., 2005
Suldal Augen gneiss, Røldal, B00127 Zrn U-Pb 1495 ±13 Bingen et al., 2005
Telemark Rjukan Gp, Vermork fm, Skardfoss rhyolite KLN7035 Zrn U-Pb 1495 ±2 Laajoki & Corfu, 2007
Suldal Sauda supracrustals, augen gneiss, B00106 Zrn U-Pb 1496 ±11 Bingen | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_26.txt | 09 16229 0.10521 1.1 4.202 1.9 0.2897 1.5 0.81 1640 22 1718 21 4.6
14 50662 0.10429 0.8 4.269 1.5 0.2969 1.3 0.86 1676 19 1702 14 1.5
15 15630 0.10335 0.9 4.231 1.7 0.2969 1.5 0.86 1676 22 1685 16 0.5
18 4993 0.10208 1.3 4. | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1167.txt | ites: implications for tectonic setting, magma source and magmatic processes at the Moho"}]}]},{"#name":"host","$$":[{"#name":"issue","$$":[{"#name":"series","$$":[{"#name":"title","$$":[{"#name":"maintitle","_":"Earth Planet. Sci. Lett."}]},{"#name":"volume-nr","_":"389"}]},{"#name":"date","_":"2014"}]},{"#name":"page... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_35.txt | 85017 Zrn U-Pb 1640 ±16 Johansson et al., 1993
North Granodiorite Ammesjön 79112 Zrn U-Pb 1645 ±9 Welin, 1994
South Migmatitic granodiorite, Viared, DC03116 Zrn U-Pb 1647 ±12 Austin Hegardt et al., 2005
South Steninge mafic dyke, Steninge, 2 Zrn U-Pb 1654 ±9 Christoffel et al., 1999
South Paleosome in orthog | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_947.txt | 25"}},{"#name":"__text__","_":"μm. Concentrations below 0.3% are considered qualitative. The full dataset "}]}]}]},{"#name":"section","$$":[{"#name":"section","$":{"xmlns:ce":true,"xmlns:mml":true,"xmlns:xs":true,"xmlns:xlink":true,"xmlns:xocs":true,"xmlns:tb":true,"xmlns:xsi":true,"xmlns:cals":true,"xmlns:sb":true,"xm... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_920.txt | s-left\"><li><span class=\"u-text-italic\">Received</span>: The date the article was originally submitted to the journal.</li><li><span class=\"u-text-italic\">Revised</span>: The date the most recent revision of the article was submitted to the journal. Dates corresponding to intermediate revisions are not shown.</li>... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_965.txt | Spaggiari"},{"#name":"cross-ref","$":{"id":"crf0060","refid":"aff0005"},"$$":[{"#name":"sup","$":{"loc":"post"},"_":"a"}]}]}],"floats":[],"footnotes":[],"attachments":[]},"title":{"content":[{"#name":"title","$":{"id":"tit0005"},"_":"Foreign contemporaries – Unravelling disparate isotopic signatures from Mesoproterozoi... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_35.txt | 52 and 1.48 Ga (Figs. 2, 7; Tables 1, 10). This event
corresponds to a major continental growth event involving formation of widespread volcanic and plutonic
complexes. Crust older than 1.52 Ga is not positively
identified, although a ca. 1.8-1.7 Ga isotopic reservoir is
allowed for by isotopic data on magmatic rocks (... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_908.txt | genesis. The generation of leucosomes and leucogranites at ca. 1030–1020 Ma, which have a more evolved Hf isotopic composition, probably reflects an even higher degree of remelting of older crust. The Hf–O isotopic patterns show that Sveconorwegian magmas differ from typical arc magmas by lower involvement of sediment... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_610.txt | div class="series"><h3 class="title">Precambrian Res.</h3></div><div class="series">(2009)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>K.E. </span>Karlstrom</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/sc... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_523.txt | -content"></div><div role="region" aria-label="Download options and search"><div class="accessbar"><div class="accessbar-label"></div><ul aria-label="PDF Options"><li class="RemoteAccess"><a class="link-button RemoteAccessButton accessbar-utility-component accessbar-utility-link link-button-primary link-button-icon-lef... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt3_150.txt | ://static.mendeley.com/view-pdf-component/0.8.9/dist/view-pdf-element.js","integratorId":{"other":8301,"accessbar":10879}},"reaxys":{"apiUrl":"https://reaxys-sdlc.reaxys.com","origin":"sciencedirect","queryBuilderHostPath":"https://www.reaxys.com/reaxys/secured/hopinto.do","url":"https://www.reaxys.com"},"oneTrustCooki... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_14.txt | OLOGY Timing of continental building in the Sveconorwegian orogen 101
distriktet Røldal-Haukelisæter-Valldalen ved Rb-Sr whole-rock
metoden, dets plass i den sørvestnorske Prekambriske Provinsen,
og en vurdering av denne provinsen i lys av det generelle
geokronologiske mønster i det Nord-Atlantiske Prekambriske
| |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_62.txt | of U-Pb dates on magmatic events in the Bamble-Kongsberg sector
Lithology, Sample Mineral - Age Reference
(1) (Ma)
Herefoss granite Zrn 920 +16/-27 Andersen et al., 2002 a
Herefoss granite, 107 Ttn 926 ±8 Andersen, 1997
Grimstad granite Zrn 989 ±9 Kullerud and Machado, 1991
Gloserheia pegmatite Eux 1060 +8/-6 Baadsgaa... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1474.txt | 51.887L41.588,37.786c3.486-4.144,5.396-9.358,5.396-14.786c0-12.682-10.318-23-23-23s-23,10.318-23,23
s10.318,23,23,23c4.761,0,9.298-1.436,13.177-4.162l13.661,14.208c0.571, | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_683.txt | ria-expanded="false"><span class="button-link-text">Show abstract</span><svg focusable="false" viewBox="0 0 92 128" width="17.25" height="24" class="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-margi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt2_7.txt | errorBeacon: o.errorBeacon,
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_34.txt | 20 4 -0.4 293 ±1 2 -0.3 15 May 03 (7) 1793 ±18 7 -0.2 2695 ±19 6 -0.2 961 ±36 7 -0.5 21 May 03 1794 ±16 4 -0.2 293 ±1 4 -0.3 02 Jun 03 1814 ±39 7 0.9 04 Jun 03 1818 ±15 4 1.2 2695 ±20 6 -0.2 06 Jun 03 (7) 1801 ±25 8 0.2 19 Jun 03 1787 ±15 7 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1075.txt | formed in a hot and slow cooling orogen."}],"$":{"view":"all","id":"sp0015"},"#name":"simple-para"}],"$":{"view":"all","id":"as015"},"#name":"abstract-sec"}],"$":{"view":"all","id":"ab015","lang":"en","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"#name":"abstracts"},"pdf... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_16.txt | . The measured isotope ratios were corrected for
element- and mass-bias effects using the Geostandard
91500 reference zircon. Common Pb detected in the analyses is mainly instrumental. A common Pb correction
was thus applied using a modern isotopic composition
(Stacey & Kramers 1975) on the basis of the 204Pb analysis.... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_53.txt | ircon data (Table 4; Bingen et al. 2008b). Amphibolite-facies deformation along the Vardefjell Shear Zone is
coeval or younger than peak metamorphism at c. 1010
Ma. Post-peak mylonitization is younger. Fabric-parallel
titanite may record continued deformation at 985 ±5 Ma
(Fig. 4; Table 5; Bingen et al. 2008b). Titanit... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_627.txt | -font-sans"><span>L.J. </span>Anderson</span><em> et al.</em></span><h3 class="title">The effect of temperature and fO<sub>2</sub> on the Al-in-hornblende barometer</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Am. Mineral.</h3></div><div class="series">(1995)</div></span></li><li... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_3.txt | Västergötland dolerite, Trollhättan Bdl U-Pb 1300 c. Söderlund et al., 2005
Göta granite, IML1 Zrn U-Pb 1304 ±6 Austin Hegardt et al., 2007
Kärra granite, DC20009 Zrn U-Pb 1311 ±8 Austin Hegardt et al., 2007
Ursand granite Zrn U-Pb 1319 ±6 Piontek et al., 1998
Stråvalla augen gneiss | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_82.txt | 14-518.
Welin, E., Gorbatschev, R. & Kähr, A.M. 1982: Zircon dating of polymetamorphic rocks in southwestern Sweden. Sveriges Geologiska
Undersökning C797, 1-34.
Welin, E. & Samuelsson, L. 1987: Rb–Sr and U–Pb isotope studies of
granitoid plutons in the Göteborg region, southwestern Sweden.
Geologiska Föreningens i Sto... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_9.txt | ite of the Rjukan group.
Norges geologiske undersøkelse Bulletin 440, 19-26.
Andersen, T. & Laajoki, K. 2003: Provenance characteristics of
Mesoproterozoic metasedimentary rocks from Telemark, South
Norway: a Nd-isotope mass-balance model. Precambrian Research
126, 95-122.
Andersen, T., Griffin, W.L., Jackson, S.E., Kn... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1420.txt | (function watchAndSetPendo(nextDelay, retryAttempt) {
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model4_15.txt | monazite and molybdenite geochronology demonstrate that the high-grade lithologies of the RogalandVest Agder Sector resided in high-grade conditions for
more than 100 million years between 1035 and 900 Ma.
Metamorphism peaked in granulite-facies conditions
first during the Agder phase between 1035 and 980 Ma
(M1 mediu... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_6.txt | U-Pb dating
of the Rogaland complex, Norway. Earth and Planetary Science
Letters 139, 335-350.
Sigmond, E.M.O. 1975: Geologisk kart over Norge, berggrunnskart
Sauda, 1:250000. Norges geologiske undersøkelse, Trondheim.
Sigmond, E.M.O. 1978: Beskrivelse til det berggrunnsgeologiske kartbladet Sauda 1:25 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1014.txt | ","class":"author"},"#name":"abstract"}],"$":{"xmlns:ce":true,"xmlns:dm":true,"xmlns:sb":true},"#name":"abstracts"},"pdf":{"urlType":null},"iss-first":"","vol-first":"265","isThirdParty":false,"language":"en","issn-primary-unformatted":"03019268","issn-primary-formatted":"0301-9268"},{"pii":"S0301926815001473","doi":"1... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1076.txt | ":"278","isThirdParty":false,"language":"en","issn-primary-unformatted":"03019268","issn-primary-formatted":"0301-9268"},{"pii":"S0301926814002551","doi":"10.1016/j.precamres.2014.07.008","journalTitle":"Precambrian Research","publicationYear":"2014","publicationDate":"2014-10-01","volumeSupText":"Volume 252","articleN... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_528.txt | 14.9 c-8.2,0-14.9,6.71-14.9,14.9v86.18l-10.08,0c-3.71,0-6.72,3.01-6.72,6.72v10.74H11.86c-3.71,0-6.72,3.01-6.72,6.72v11.68h243.62 v-11.63C248.77,229.45,245.78,226.43 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_313.txt | -pc-sdk.ot-vs-list.ot-vnd-serv-hdr-cntr.ot-vnd-serv-hdr,#onetrust-pc-sdk.ot-vnd-serv.ot-vnd-serv-hdr-cntr.ot-vnd-serv-hdr{font-weight:600;font-size:.95em;line-height:2;margin-left:.5rem}#onetrust-pc-sdk.ot-vs-list.ot | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_625.txt | ="series">(2014)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="u-font-sans"><span class="author u-font-sans"><span>G. </span>Viola</span><em> et al.</em></span><h3><a class="anchor title anchor-default" href="/science/article/pii/S0301926811001380" target="_self"><span class="anchor-text">Th... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_713.txt | bottom"><button class="button-link related-content-panel-toggle is-up button-link-primary button-link-icon-right" type="button" aria-expanded="true"><span class="button-link-text"><h2 class="section-title u-h4"><span class="related-content-panel-title-text">Part of special issue</span></h2></span><svg focusable="false"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1481.txt | class="ot-label-status">label</span></div></div></div><div class="ot-fltr-btns"><button id="filter-apply-handler">Apply</button> <button id="filter-cancel-handler">Cancel</button></div></div></div></section></div></div><section id="ot-lst-cnt" class="ot-host-cnt ot-pc-scrollbar"><div id="ot-sel-blk"><div class="ot-sel... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_28.txt | 0.2347 2.0 0.92 1359 24 1676 15 19
16 19066 0.10417 1.0 3.863 2.2 0.2690 2.0 0.90 1536 28 1700 18 9.7
08p 2656 0.10593 1.5 3.935 1.9 0.2695 1.2 0.61 1538 16 1730 28 11
11p 3711 0.10380 0.9 3.975 1.7 0.2777 1.4 0.85 1580 20 | |
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