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no_hydrocarbons_in_sveconorwegian_belt/Petroleum_trap1.txt | part1 -------------------
In petroleum geology, a trap is a geological structure affecting the reservoir rock and caprock of a petroleum system allowing the accumulation of hydrocarbons in a reservoir. Traps can be of two types: stratigraphic or structural. Structural traps are the most important type of trap as they r... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_776.txt | Belt (SMB). Previously mapped as granitic gneisses in many areas, the existence of this large, commonly undeformed and unmetamorphosed granitoid batholith was only recognized a few years ago ("},{"$":{"id":"crf0160","refid":"bib0275"},"#name":"cross-ref","_":"Slagstad et al., 2013a"},{"#name":"__text__","_":"). Magmat... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_710.txt | 45 45-45 45z"></path></svg></span><span class="button-alternative-text">View all citing articles on Scopus</span><svg focusable="false" viewBox="0 0 78 128" aria-label="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.... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_6.txt | of Geology vol.
88, pp 43-72. Trondheim 2008. ISSN 029-196X.
The Sveconorwegian orogenic belt resulted from collision between Fennoscandia and another major plate, possibly Amazonia, at the end of the
Mesoproterozoic. The belt divides, from east to west, into a Paleoproterozoic Eastern Segment, and four mainly Mesopro... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing2_13.txt | complex
and the supracrustal rocks are conformable. Fine-grained
rocks interpretable as metavolcanic rocks are common
in the gneiss complex. Three samples of this gneiss
complex, namely an augen gneiss (sample B00-137), a
weakly deformed K-feldspar megacrystic granite gneiss
(sample B00-112) and a weakly deformed gran... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_864.txt | oo A., Skridlaite G., Krzeminska E., Shumlyanskyy L., Holland M.E., Holm-Denoma C., Teixeira W., Faleiros F.M., Ribeiro B.V., Jacobs J., Wang C., Thomas R.J., Macey P.H., Kirkland C.L., Hartnady M.I.H., Eglington B.M., Puetz S.J., Condie K.C.","doi":"10.1016/j.precamres.2021 | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_28.txt | , district of
Keewatin, Northwest Territories. Radiogenic age and isotopic studies:
report 11; Geological Survey of Canada, Current research 1998-F, 81-88.
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 Shield. The Journal o... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_34.txt | 10269 0.7 4.290 1.4 0.3030 1.2 0.84 1706 18 1673 14 -2.0
05 122367 0.10487 0.9 4.387 1.6 0.3034 1.3 0.84 1708 20 1712 16 0.2
FUN38, granitic gneiss
01p 11497 0.10346 0.7 3.882 2.0 0.2721 1.9 0.93 1552 26 1687 14 8.0
04p 33572 0 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing1_39.txt | sen et al. 1997; Åhäll et al. 1998; de Haas
et al. 1999; Bingen et al. 2001a). The Bamble-Kongsberg
sector displays gabbro and granitoid metaplutons
intruded between 1.20 and 1.15 Ga and late-Sveconorwegian granite plutons formed between 1.00 and
0.92 Ga (Table 9, Fig. 7C).
Telemark sector
The Telemark sector occurs to... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing4_37.txt | Sand granodiorite weak B00-139 353257 6594411 Amp, Bt, Ttn LA-ICPMS 12 12 1.4 1506 13 intrusion 10G
Ølen Aurdal granite weak R94-66 314950 6607000 Bt, Ms ID-TIMS 3 3 0.56 1506 2 intrusion 8G
Sauda Vanvik augen gneiss weak B00-112 345527 6600998 Bt LA-ICPMS 8 8 0.76 1516 11 intrusion 10F
| |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_33.txt | -crustal levels, with metamorphism ranging from low-grade to granulite-facies.
The Hardangervidda Sector consists of amphibolitefacies gneisses with a general E-W structural grain
(Sigmond 1998). The Suldal Sector is characterized by
greenschist- to epidote-amphibolite-facies supracrustal
sequences, associated with plu... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_67.txt | Bingen et al. 2005;
Laajoki & Corfu 2007), is coeval with the volumetrically
minor 1530-1500 Ma Ragunda rapakivi granite suite in
western Fennoscandia (Persson 1999; Åhäll et al. 2000;
Andersson et al. 2002b). The 1280-1260 Ma continental bimodal magmatic suite associated with clastic sediments in the Suldal Sector (Bi... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_94.txt | , i, e, t, r);
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_500.txt | .95h3.93V6.97h-3.93V2.97h-2.48v3.99h-2.71v1.98h2.71v9.67c0 2.64 1.39 3.73 3.33 3.73 1.15 0 2.54-0.39 3.43-0.79L170 19.44M173.68 5.96c-1.09 0-2-0.87-2-1.97 0-1.1 0.91-1 | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_36.txt | .065 1.5 0.2833 1.3 0.85 1608 18 1698 15 5.3
20p 8096 0.10291 0.8 4.029 1.6 0.2839 1.4 0.86 1611 20 1677 15 3.9
12p 5419 0.10385 0.9 4.068 1.6 0.2841 1.3 0.84 1612 19 1694 16 4.8
05 37174 0.10541 0.9 4.171 1.5 0. | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_19.txt | al., 2005
Göteborg suite, Kil tonalite Zrn U-Pb 1607 ±4 Åhäll & Connelly, 2008
Göteborg batholith, Frykdalshöjden orthogneiss Zrn U-Pb 1608 ±4 Åhäll & Connelly, 2008
Höjen tonalite, SWS8 Zrn U-Pb 1609 +35/-25 Persson et al., 1983
Åmål Fm, Tösse porphyry Zrn | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_39.txt | Association of Canada,
Special Paper 38.
Johansson, Å., Meier, M., Oberli, F. & Wikman, H. 1993: The early
evolution of the Southwest Swedish Gneiss Province: geochronological and isotopic evidence from southernmost Sweden. Precambrian Research 64, 361-388.
Kiel, H.M., Cornell, D.H. & Whitehouse, M.J. 2003: Age and em... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1121.txt | relationships. The main facies, mostly charnockitic, contains orthopyroxene whereas a subordinate granitic facies comprises hornblende and biotite. U–Pb (zircon) isotopic data show overlapping ages of 931"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__text__","_":"±"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"__tex... | |
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no_hydrocarbons_in_sveconorwegian_belt/Kerogen4.txt | part4 -------------------
Microstructure[edit]
The microstructure of kerogen also evolves during thermal maturation, as has been inferred by scanning electron microscopy (SEM) imaging showing the presence of abundant internal pore networks within the lattice of thermally mature kerogen. Analysis by gas sorption demonst... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_79.txt | , Ullared, N049 U-Pb SIMS 4 Johansson et al., 2001 South Zrn 968±13 Am Migmatitic Torpa granite, TA1 U-Pb SIMS 10 Andersson et al., 2002 South Zrn 969±13 Am Migmatitic banded orthogneiss, Skene gneiss, SE-1 U-Pb SIMS 14 Andersson et al., 2002 South Zrn 969±27 Am Glassvik deformed pegmatite dyke Pb-Pb TIMS 4 Söderlund | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_49.txt | orwegian thrusting of the
Bamble-Kongsberg sector over the Telemark sector
(Starmer 1985; Andersson et al. 1996; Henderson &
Ihlen 2004; Ebbing et al. subm). The cover of clastic
sediments younger than 1.12 Ga over the Telemark sector, namely the Heddal group and Eidsborg formation
(de Haas et al. 1999; Laajoki et al. ... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_767.txt | ":"The Sirdal Magmatic Belt (SMB) is a newly discovered Sveconorwegian (ca. 1060–1020"},{"$":{"sp":"0.25"},"#name":"hsp"},{"#name":"text","$$":[{"#name":"__text__","_":"Ma) granite "},{"#name":"topic-link","_":"batholith","$":{"href":"/topics/earth-and-planetary-sciences/batholith","term":"batholith"}},{"#name":"__text... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_19.txt | ).
Geochronological data give evidence for two metamorphic phases (Tables 4, 5). The first phase at 1140-1125
Ma is limited to the Bamble Terrane. It is recorded in
amphibolite-facies and granulite-facies rocks by zircon at
1125 ±46 and 1124 ±8 Ma (Knudsen et al. 1997b; Knudsen & Andersen 1999), by monazite ranging fro... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_15.txt | 235U 238U 206Pb 238U
(Ma) (Ma) (%)
(1) (1) (1) (2) (3
15 0.0940 0.0008 2.94 0.04 0.227 0.003 0.82 1508 16 1317 15 87.3
3 0.0944 0.0008 2.99 0.04 0.230 0.003 0.79 1516 16 1333 13 87.9
B00-112, augen gneiss, Vanvik, Fig. 10F
| |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_517.txt | 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 17.97-11.97 28 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_57.txt | Feiring quartz diorite, Ø3 Zrn 1574 ±17 Andersen et al., 2004
Idala tonalite Zrn 1584 ±15 Åhäll et al., 1995
Bjørkelangen granodiorite, TA118 Zrn 1585 ±18 Andersen et al., 2004
Bua gneiss, TK1-TK2 Zrn 1585 ±11 Andersson et al., 2002
Rönnäng tonalite Zrn 1587 ±3 Connelly and Åhäll, 1996
| |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_84.txt | mean age calculation.
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 109
110 B. Bingen et al. NORWEGIAN JOURNAL OF GEOLOGY
Table 5. LA-ICPMS U-Pb data on zircon from orthogneiss samples
Atomic ratios Ages
Sample/ 207Pb ±σ 207Pb ±σ 206Pb ±σ rho 207Pb ±σ 206Pb ±σ Disc.
analysis ... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_35.txt |
migmatitization (Rygnestad locality; Fig. 4; Table 4; Bingen et al. 2008b).
The central part of the Telemark sector is made up of lowgrade supracrustal rocks (Fig. 4). In these rocks, original
stratigraphic relationships and textures are extensively
preserved (Dons 1960). Four main stratiform sequences,
separated by u... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_647.txt | veconorwegian orogenic belt, a case of late-proterozoic plate-collision</h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Geol. Rundsch.</h3></div><div class="series">(1980)</div></span></li><li class="bib-reference u-margin-s-bottom"><span class="author u-font-sans"><span>T. </span>F... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_616.txt | 14004488" target="_self"><span class="anchor-text">Developing an inverted Barrovian sequence; insights from monazite petrochronology</span></a></h3><span class="host u-clr-grey6 u-font-sans"><div class="series"><h3 class="title">Earth Planet. Sci. Lett.</h3></div><div class="series">(2014)</div></span></li><li class="b... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_1164.txt | name":"date","_":"2004"}]},{"#name":"pages","$$":[{"#name":"first-page","_":"249"},{"#name":"last-page","_":"273"}]}]}]}]},{"#name":"bib-reference","$":{"id":"bib0065"},"$$":[{"#name":"label","_":"Bybee et al., 2014"},{"#name":"reference","$":{"id":"sbref0065","refId":"13"},"$$":[{"#name":"contribution","$":{"langtype"... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_929.txt | 60 and 1020"},{"#name":"hsp","$":{"sp":"0.25"}},{"#name":"__text__","_":"Ma (Slagstad et al., 2013a; this work). The purpose of this paper is to present new field, petrological and geochronological data from the SMB, as well as from para- and orthogneiss xenoliths within and forming the host rocks of the SMB. These dat... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_583.txt | veconorwegian 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<!-- --... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_30.txt | 2007b). The Telemarkia Terrane is the location of voluminous Sveconorwegian plutonism, including 1050-1035
Ma granodiorite to granite suites, 1030-1000 Ma syn-collisional granitoids, 970-930 Ma post-collisional monzodiorite to granite plutons, and the 930-920 Ma Rogaland
anorthosite-mangerite-charnockite (AMC) complex
... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_856.txt | #name":"para","_":"The distribution of UHT rocks reflects differential tectonic exhumation."}],"$":{"id":"o0015"},"#name":"list-item"},{"$$":[{"#name":"label","_":"•"},{"$":{"view":"all","id":"p0020"},"#name":"para","_":"At no point during orogeny did the crust in the study area thicken significantly."}],"$":{"id":"o00... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing5_59.txt | 96 ±11 Larson et al., 1999
Tistedal granodiorite, Ø1 Zrn 1599 +15/-16 Andersen et al., 2004
Lerum granite, 76263 Zrn 1603 ±40 Welin and Samuelsson, 1987
Stora Lundby granodiorite, mesosome 9701b Zrn 1605 ±10 Scherstén et al., 2004
Höjen tonalite, SWS8 Zrn 1609 +35/-25 Persson et al., 1983
Åmål fm, Tös | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_31.txt | ys et al., 2002
South Deformed granitic dyke, Gällared S Zrn U-Pb 1443 ±26 Söderlund et al., 2002
South Beden granodiorite, Romeleåsen, 85016 Zrn U-Pb 1449 +23/-11 Johansson et al., 1993
South Charnockite, NW of Örkelljunga, 85019 Zrn U-Pb 1452 c. Johansson et al., 1993
South Aplitic dyke, post-S2 pre-S | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt1_33.txt | spa: {
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no_hydrocarbons_in_sveconorwegian_belt/building_timing4_13.txt | lund, P., Söderlund, U., Möller, C., Gorbatschev, R. & Rodhe, A.
2004: Petrology and ion microprobe U-Pb chronology applied to a
metabasic intrusion in southern Sweden: a study on zircon
formation during metamorphism and deformation. Tectonics 23,
TC5005, doi:10.1029 /2003TC001498.
Söderlund, U. 1996: Conventional U-Pb... | |
no_hydrocarbons_in_sveconorwegian_belt/building_timing3_48.txt | Mesoproterozoic anorogenic magmatism in southern Norway. In Brewer, T.S. (ed.), Precambrian
crustal evolution in the North Atlantic Region. Geological Society,
London, Special Publications, 112, 275-295.
Mortensen, O. 1942: Et eruptivfelt i Kvinnherad og Skånevik herreder.
Bergens Museum Årbok, Naturvitenskapelig rekk... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_702.txt | =citing-articles:type=view-details" aria-describedby="citing-articles-article-5-title" aria-controls="citing-articles-article-5" aria-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... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model3_31.txt | ; Schärer et
al. 1996; Bingen & van Breemen 1998a; Schiellerup et
al. 2000; Andersen et al. 2001; Bogaerts et al. 2003; Bolle
et al. 2003a; Vander Auwera et al. 2003; Andersen et al.
2007b). Undeformed c. 850 Ma mafic dykes post-date
regional cooling (Walderhaug et al. 1999).
For descriptive purposes, the Telemarkia Te... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model2_59.txt | ±3, 907±5 Am Augen gneiss, Sirdal, B185 U-Pb ID-TIMS 4 Bingen & van Breemen, 1998
Rogaland-VA Mnz 999±5, 922±5 Am Augen gneiss, Feda, B135 Th-Pb ID-TIMS 2 Bingen et al., 2008
Rogaland-VA Mnz 1010±2, 1000±1, 930±1, 928±1 Am Augen gneiss, Feda, B135 | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt5_74.txt | IndexOf(':');
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no_hydrocarbons_in_sveconorwegian_belt/building_timing2_23.txt | gneiss complex. The lithologies in the
sampled section of the Botsvatn gneiss complex are similar to lithologies recorded in the nearby Grjotdokki-Nesflaten supracrustal rocks,
except for the presence of a much larger volume of leucosome in the
gneiss complex. The data available today are consistent with a nearcoeval ... | |
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no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_651.txt | ="17.25" height="24" class="icon icon-navigate-down u-fill-grey8"><path d="m1 51l7-7 38 38 38-38 7 7-45 45z"></path></svg></span><span class="button-alternative-text">View more references</span></button></div></div><div id="preview-section-cited-by"><section aria-label="Cited by" class="ListArticles preview"><div class... | |
no_hydrocarbons_in_sveconorwegian_belt/late_mesoproterozoic_sirdal_magmatic_belt4_506.txt | -help-icon-popover"><input type="hidden"><button class="button-link gh-nav-help-icon gh-icon-btn button-link-primary button-link-icon-only" type="button" aria-expanded="false" aria-label="ScienceDirect Support Center links"><svg focusable="false" viewBox="0 0 114 128" aria-hidden="true" alt="ScienceDirect help page" wi... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_44.txt | (Ma)
(1) (2) (2) (2) (3) (4) (5) (6) (6) (6)
N9438. granite
1 3 13 15.8 75 1 1.61 9615 0.06999 6 1.49288 243 0.15470 24 928.0 1.7
2 3 9 18.3 83 5 1.86 1451 0.07007 15 1.49235 388 0.15449 28 930.5 4.4
3 1 5 12.9 62 | |
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no_hydrocarbons_in_sveconorwegian_belt/building_timing5_37.txt | presented in this study
NORWEGIAN JOURNAL OF GEOLOGY Timing of continental building in the Sveconorwegian orogen 113
Table 7. Selection of U-Pb dates on magmatic events in the Eastern Segment
Lithology, Sample Mineral - Age Reference
(1) (Ma)
Riddaho rare-mineral pegmatite Clm 942 ±2 Romer and Smeds, 1996
Vaggeryd sye... | |
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no_hydrocarbons_in_sveconorwegian_belt/4phrase_model5_1.txt | 2003b: Magnetic fabrics in the
Holum granite (Vest-Agder, southernmost Norway): implications
for the late evolution of the Sveconorwegian (Grenvillian) orogen
of SW Scandinavia. Precambrian Research 121, 221-249.
Brewer, T.S., Daly, J.S. & Åhäll, K.I. 1998: Contrasting magmatic arcs in
the Palaeoproterozoic of the sou... | |
no_hydrocarbons_in_sveconorwegian_belt/4phrase_model1_30.txt | p 18003 0.10451 0.9 4.068 1.8 0.2823 1.5 0.85 1603 21 1706 17 6.0
19p 2441 0.10289 1.0 4.023 1.7 0.2836 1.4 0.80 1609 19 1677 19 4.0
14 20798 0.10561 1.0 4.148 1.7 0.2849 1.4 0.82 1616 20 1725 18 6.3
23p 5804 0.10305 0. | |
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