Fergusson, Christopher L (2003): (Table T1) Mineral composition of turbidite sands and sandstones from ODP Leg 190 sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.779594, Supplement to: Fergusson, CL (2003): Provenance of Miocene-Pleistocene turbidite sands and sandstones, Nankai Trough, Ocean Drilling Program Leg 190. In: Mikada, H; Moore, GF; Taira, A; Becker, K; Moore, JC; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 190/196, 1-28, https://doi.org/10.2973/odp.proc.sr.190196.205.2003
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Abstract:
During Ocean Drilling Program Leg 190 several turbidite successions in the Nankai Trough were drilled through including Pleistocene trench fill (Sites 1173 and 1174), Pleistocene-Pliocene slope basin deposits and underlying trench fill (Sites 1175 and 1176), Miocene Shikoku Basin deposits (Site 1177), and upper Miocene trench fill (Site 1178). Sands from the Pleistocene trench-fill succession of the Nankai Trough are of mixed derivation with significant monomineralic components (quartz and feldspar) and mafic to intermediate volcanic rock fragments, in addition to sedimentary and less abundant metamorphic detritus. They have a source in the Izu collision zone in central Honshu. Sands from the slope and accreted trench fill at Sites 1175 and 1176 are dominated by quartz with less abundant feldspar, sedimentary rock fragments, and only minor volcanic and metamorphic rock fragments. In contrast to the trench turbidites of Sites 1173 and 1174, these sands are very quartzose with characteristic radiolarian chert fragments. Volcanic rock fragments are mainly of silicic composition. Potential sources of these sands are uplifted subduction complexes of southwest Japan. Sands from the accreted trench turbidites at Site 1178 have clast types similar to those at Sites 1175 and 1176. In contrast, however, framework detrital modes are distinctive, with Site 1178 sands having substantially lower total quartz contents and more abundant fine-grained sedimentary rock fragments. These sands were also probably derived from the island of Shikoku, but their composition indicates that sedimentary rocks were abundant in the source area and these may have been Miocene forearc basin successions that were largely removed by erosion. Erosional remnants of Miocene forearc basin deposits are present on the Kii Peninsula east-northeast of Shikoku. Erosion followed a phase of exhumation of the Shimanto Belt indicated by apatite fission track ages at ~10 Ma. Sand in the lower-upper Miocene turbidites of the lower Shikoku Basin section at Site 1177 is more varied in composition, with the upper part of the unit similar to Site 1178 (i.e., rich in sedimentary rock fragments) and the lower part similar to those at Sites 1175 and 1176 (i.e., rich in quartz with some silicic volcanic rock fragments). Sands from the lower part of the Miocene turbidite unit were derived from a continental source with plutonic and volcanic rocks, possibly the inner zone of southwest Japan.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: 32.425076 * Median Longitude: 134.599173 * South-bound Latitude: 31.652510 * West-bound Longitude: 134.011880 * North-bound Latitude: 32.731010 * East-bound Longitude: 134.956460
Date/Time Start: 2000-05-07T17:30:00 * Date/Time End: 2000-07-15T13:25:00
Minimum Elevation: -4844.3 m * Maximum Elevation: -1741.7 m
Event(s):
190-1174A * Latitude: 32.342300 * Longitude: 134.956460 * Date/Time Start: 2000-06-07T07:00:00 * Date/Time End: 2000-06-09T13:30:00 * Elevation: -4751.2 m * Penetration: 74.1 m * Recovery: 47.04 m * Location: Philippine Sea * Campaign: Leg190 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 74.1 m cored; 0 m drilled; 63.5 % recovery
190-1174B * Latitude: 32.342330 * Longitude: 134.956430 * Date/Time Start: 2000-06-09T01:30:00 * Date/Time End: 2000-06-22T22:30:00 * Elevation: -4751.2 m * Penetration: 1119.8 m * Recovery: 577.57 m * Location: Philippine Sea * Campaign: Leg190 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 102 cores; 976.1 m cored; 143.7 m drilled; 59.2 % recovery
190-1175A * Latitude: 32.598080 * Longitude: 134.644580 * Date/Time: 2000-06-22T22:30:00 * Elevation: -2997.5 m * Penetration: 445 m * Recovery: 327.01 m * Location: Philippine Sea * Campaign: Leg190 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 47 cores; 439.2 m cored; 5.8 m drilled; 74.5 % recovery
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
1716 data points
Data
1 Event | 2 Sample label (DSDP/ODP/IODP sample designation) | 3 Sample ID | 4 MonoQz [%] (Point counting) | 5 MonoQz [%] (with undulose extinction, Poi...) | 6 PolyQz [%] (Point counting) | 7 PolyQz [%] (with a planar fabric, Point c...) | 8 Chert [%] (Point counting) | 9 Pl [%] (Point counting) | 10 Kfs [%] (Point counting) | 11 Lithic [%] (sedimentary, Point counting) | 12 Lithic [%] (felsitic volcanic, Point coun...) | 13 Lithic [%] (mafic intermediate felsitic v...) | 14 Lithic [%] (volcanic glass, Point counting) | 15 Lithic [%] (volcanic tube pumice, Point c...) | 16 Lithic [%] (total volcanic, Point counting) | 17 Lithic [%] (metasedimentary, Point counting) | 18 Lithic [%] (metavolcanic, Point counting) | 19 Lithic [%] (unidentified meta, Point coun...) | 20 Lithic [%] (plutonic, Point counting) | 21 Bt [%] (Point counting) | 22 Chl [%] (Point counting) | 23 Ep [%] (Point counting) | 24 Grt [%] (Point counting) | 25 Hbl [%] (Point counting) | 26 Ms [%] (Point counting) | 27 Opaque [%] (Point counting) | 28 Pyrox [%] (including olivine, Point coun...) | 29 Tur [%] (Point counting) | 30 Zrn [%] (Point counting) | 31 Sum [%] (Point counting) | 32 Carb (raw count, Point counting) | 33 OM (raw count, Point counting) | 34 Qz [%] (Point counting) | 35 Fsp [%] (Point counting) | 36 Lithic [%] (total, Point counting) | 37 Metam fragm [%] (of total lithics, Point counting) | 38 Volcanic [%] (of total lithics, Point counting) | 39 Sed fragm [%] (of total lithics, Point counting) | 40 Ratio ((Chert + Quartz polycr)/Quart...) | 41 Pl/Fsp (Point counting) | 42 Ratio (volcanic lithics/total lithic...) | 43 MonoQz [%] (of total Monoquartz+Kfsp+Plag...) | 44 Kfs [%] (of total Monoquartz+Kfsp+Plag...) | 45 Pl [%] (of total Monoquartz+Kfsp+Plag...) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
190-1174A | 190-1174A-3H-5,69-73 | 43 | 8.2 | 8.6 | 4.0 | 0.0 | 0.4 | 18.6 | 3.6 | 18.4 | 6.0 | 19.4 | 0.0 | 0.0 | 25.4 | 4.8 | 1.8 | 1.2 | 1.6 | 0.2 | 0.0 | 1.4 | 0.0 | 0.2 | 0.0 | 0.0 | 1.6 | 0.0 | 0.0 | 100 | 1 | 0 | 21.9 | 23.0 | 55.1 | 15.1 | 49.2 | 35.7 | 0.21 | 0.84 | 0.48 | 27.0 | 11.8 | 61.2 |
190-1174A | 190-1174A-8H-5,55-60 | 46 | 3.8 | 5.4 | 2.0 | 0.0 | 0.2 | 16.2 | 1.2 | 17.6 | 7.4 | 38.2 | 0.0 | 0.0 | 45.6 | 3.0 | 0.0 | 0.8 | 0.4 | 0.0 | 0.0 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 3.4 | 0.0 | 0.0 | 100 | 2 | 0 | 11.9 | 18.1 | 70.1 | 5.7 | 68.1 | 26.3 | 0.19 | 0.93 | 0.68 | 17.9 | 5.7 | 76.4 |
190-1174A | 190-1174A-8H-CC,0-3 | 48 | 3.8 | 6.6 | 0.8 | 0.0 | 0.4 | 17.0 | 2.2 | 17.6 | 7.8 | 35.6 | 0.6 | 0.0 | 44.0 | 2.4 | 1.0 | 0.6 | 0.4 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 3.0 | 0.0 | 0.0 | 100 | 1 | 0 | 12.0 | 19.8 | 68.2 | 6.1 | 67.1 | 26.8 | 0.10 | 0.89 | 0.67 | 16.5 | 9.6 | 73.9 |
190-1174A | 190-1174A-8H-CC,10-15 | 49 | 4.0 | 4.4 | 2.0 | 0.0 | 0.4 | 17.8 | 2.2 | 20.2 | 3.0 | 34.8 | 0.4 | 0.0 | 38.2 | 1.4 | 1.8 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.2 | 7.0 | 0.0 | 0.0 | 100 | 1 | 0 | 11.7 | 21.6 | 66.7 | 5.2 | 62.0 | 32.8 | 0.22 | 0.89 | 0.62 | 16.7 | 9.2 | 74.2 |
190-1174B | 190-1174B-1R-1,6-10 | 410 | 2.0 | 1.4 | 1.4 | 0.0 | 1.8 | 18.2 | 1.8 | 32.0 | 1.2 | 33.4 | 0.0 | 0.0 | 34.6 | 2.4 | 1.4 | 0.6 | 0.2 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.2 | 1.8 | 0.0 | 0.0 | 100 | 1 | 0 | 6.7 | 20.4 | 72.8 | 6.2 | 48.7 | 45.1 | 0.48 | 0.91 | 0.49 | 9.1 | 8.2 | 82.7 |
190-1174B | 190-1174B-9R-2,108-112 | 412 | 3.2 | 5.0 | 1.2 | 0.0 | 0.0 | 17.2 | 2.8 | 21.8 | 2.4 | 37.0 | 0.8 | 0.0 | 40.2 | 1.0 | 2.2 | 1.6 | 0.0 | 0.4 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.2 | 2.6 | 0.4 | 0.0 | 100 | 0 | 1 | 9.8 | 20.8 | 69.4 | 7.2 | 60.2 | 32.6 | 0.13 | 0.86 | 0.60 | 13.8 | 12.1 | 74.1 |
190-1175A | 190-1175A-37X-1,88-90 | 524 | 21.6 | 24.0 | 13.0 | 0.2 | 12.4 | 5.2 | 8.2 | 10.8 | 2.4 | 0.4 | 0.0 | 0.0 | 2.8 | 0.4 | 0.0 | 0.4 | 1.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 3 | 1 | 71.2 | 13.4 | 15.4 | 5.6 | 19.4 | 75.0 | 0.36 | 0.39 | 0.18 | 61.7 | 23.4 | 14.9 |
190-1175A | 190-1175A37X-4,30-32 | 525 | 27.2 | 18.2 | 15.0 | 0.0 | 8.8 | 4.2 | 7.2 | 15.2 | 2.8 | 0.0 | 0.0 | 0.0 | 2.8 | 1.0 | 0.0 | 0.0 | 0.2 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 8 | 1 | 69.3 | 11.4 | 19.2 | 5.3 | 14.7 | 80.0 | 0.34 | 0.37 | 0.15 | 70.5 | 18.7 | 10.9 |
190-1175A | 190-1175A-43X-3,75-78 | 534 | 28.6 | 17.0 | 8.0 | 0.0 | 5.0 | 7.2 | 11.4 | 16.4 | 3.0 | 0.0 | 0.2 | 0.0 | 3.2 | 2.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.6 | 0.2 | 0.0 | 0.0 | 0.0 | 0.4 | 0.0 | 0.0 | 100 | 0 | 1 | 59.3 | 18.8 | 21.9 | 9.3 | 14.8 | 75.9 | 0.22 | 0.39 | 0.15 | 60.6 | 24.2 | 15.3 |
190-1175A | 190-1175A-43X-3,123-126 | 535 | 26.6 | 24.8 | 9.2 | 0.6 | 3.6 | 5.2 | 7.6 | 19.0 | 1.2 | 0.2 | 0.0 | 0.0 | 1.4 | 1.0 | 0.2 | 0.2 | 0.2 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 100 | 0 | 0 | 65.1 | 12.9 | 22.1 | 6.4 | 6.4 | 87.2 | 0.20 | 0.41 | 0.06 | 67.5 | 19.3 | 13.2 |
190-1175A | 190-1175A47X-CC,3-7 | 538 | 26.8 | 21.6 | 11.2 | 0.0 | 3.0 | 3.4 | 6.0 | 23.6 | 1.0 | 0.2 | 0.0 | 0.0 | 1.2 | 2.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.2 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 0 | 5 | 63.0 | 9.5 | 27.6 | 9.5 | 4.4 | 86.1 | 0.23 | 0.36 | 0.04 | 74.0 | 16.6 | 9.4 |
190-1176A | 190-1176A32X-CC,7-9 | 613 | 23.8 | 21.6 | 8.8 | 0.4 | 5.2 | 4.6 | 7.8 | 20.2 | 2.8 | 0.4 | 0.0 | 0.0 | 3.2 | 2.4 | 0.6 | 0.0 | 0.6 | 0.0 | 0.0 | 0.4 | 0.0 | 0.2 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 0 | 0 | 60.3 | 12.5 | 27.2 | 11.4 | 12.1 | 76.5 | 0.23 | 0.37 | 0.12 | 65.7 | 21.5 | 12.7 |
190-1176A | 190-1176A-33X-CC,39-41 | 614 | 26.0 | 18.6 | 7.2 | 0.0 | 2.8 | 9.4 | 12.0 | 15.8 | 2.8 | 0.0 | 0.0 | 0.0 | 2.8 | 3.2 | 0.4 | 0.8 | 0.0 | 0.0 | 0.0 | 0.8 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 0 | 3 | 55.2 | 21.6 | 23.2 | 19.1 | 12.2 | 68.7 | 0.18 | 0.44 | 0.12 | 54.9 | 25.3 | 19.8 |
190-1176A | 190-1176A34X-CC,5-8 | 615 | 26.6 | 18.0 | 9.4 | 0.0 | 3.8 | 7.2 | 14.0 | 13.0 | 3.8 | 0.8 | 0.0 | 0.0 | 4.6 | 2.0 | 0.0 | 1.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 100 | 12 | 21 | 57.9 | 21.2 | 20.8 | 15.4 | 22.1 | 62.5 | 0.23 | 0.34 | 0.22 | 55.6 | 29.3 | 15.1 |
190-1176A | 190-1176A-35X-1,35-39 | 616 | 21.2 | 22.8 | 13.0 | 0.0 | 12.6 | 4.0 | 6.6 | 14.4 | 3.4 | 0.2 | 0.0 | 0.0 | 3.6 | 1.8 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 3 | 3 | 69.6 | 10.6 | 19.8 | 9.1 | 18.2 | 72.7 | 0.37 | 0.38 | 0.18 | 66.7 | 20.8 | 12.6 |
190-1176A | 190-1176A-36X-2,35-38 | 617 | 13.6 | 25.0 | 11.4 | 0.0 | 11.8 | 4.2 | 7.4 | 19.4 | 5.8 | 0.4 | 0.0 | 0.0 | 6.2 | 0.8 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 100 | 12 | 5 | 61.9 | 11.6 | 26.5 | 3.0 | 23.5 | 73.5 | 0.38 | 0.36 | 0.23 | 54.0 | 29.4 | 16.7 |
190-1176A | 190-1176A-40X-1,43-46 | 618 | 23.4 | 18.0 | 10.6 | 0.0 | 14.4 | 5.0 | 5.0 | 13.2 | 5.8 | 1.4 | 0.0 | 0.0 | 7.2 | 2.4 | 0.0 | 0.2 | 0.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 3 | 4 | 66.4 | 10.0 | 23.6 | 11.3 | 31.3 | 57.4 | 0.38 | 0.50 | 0.31 | 70.1 | 15.0 | 15.0 |
190-1176A | 190-1176A-40X-1,43-46 | 622 | 24.4 | 20.2 | 6.0 | 0.0 | 4.0 | 11.6 | 12.0 | 16.2 | 1.4 | 0.0 | 0.0 | 0.0 | 1.4 | 3.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.4 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 100 | 3 | 17 | 55.2 | 23.8 | 21.0 | 15.4 | 6.7 | 77.9 | 0.18 | 0.49 | 0.07 | 50.8 | 25.0 | 24.2 |
190-1176A | 190-1176A-44X-CC,34-38 | 631 | 32.4 | 21.4 | 8.8 | 0.0 | 6.2 | 5.8 | 10.2 | 9.8 | 2.4 | 0.2 | 0.0 | 0.0 | 2.6 | 1.8 | 0.0 | 0.2 | 0.2 | 0.0 | 0.0 | 0.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 5 | 69.2 | 16.1 | 14.7 | 13.9 | 18.1 | 68.1 | 0.22 | 0.36 | 0.18 | 66.9 | 21.1 | 12.0 |
190-1176A | 190-1176A-46X-CC,19-23 | 633 | 8.8 | 22.2 | 15.4 | 1.0 | 23.2 | 2.2 | 3.2 | 19.2 | 3.2 | 0.6 | 0.0 | 0.2 | 4.0 | 0.4 | 0.0 | 0.0 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 17 | 7 | 70.6 | 5.4 | 24.0 | 1.7 | 16.9 | 81.4 | 0.55 | 0.41 | 0.17 | 62.0 | 22.5 | 15.5 |
190-1176A | 190-1176A-48X-CC,14-17 | 634 | 16.8 | 24.6 | 20.0 | 0.6 | 10.0 | 4.2 | 5.4 | 13.2 | 2.4 | 0.6 | 0.0 | 0.0 | 3.0 | 1.2 | 0.0 | 0.2 | 0.8 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 4 | 6 | 72.0 | 9.6 | 18.4 | 8.0 | 17.0 | 75.0 | 0.42 | 0.44 | 0.16 | 63.6 | 20.5 | 15.9 |
190-1177A | 190-1177A-16R-5,8-10 | 71 | 15.2 | 19.8 | 6.4 | 0.0 | 2.6 | 15.2 | 9.0 | 27.6 | 2.8 | 0.4 | 0.0 | 0.0 | 3.2 | 0.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.2 | 0.0 | 100 | 0 | 2 | 44.2 | 24.3 | 44.2 | 1.9 | 10.2 | 87.9 | 0.20 | 0.63 | 0.10 | 38.6 | 22.8 | 38.6 |
190-1177A | 190-1177A-17R-1,52-56 | 73 | 8.8 | 21.0 | 4.2 | 0.0 | 2.0 | 10.8 | 9.6 | 35.6 | 5.4 | 0.0 | 0.2 | 0.0 | 5.6 | 1.6 | 0.0 | 0.2 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 2 | 9 | 36.1 | 20.4 | 43.5 | 4.2 | 13.0 | 82.8 | 0.17 | 0.53 | 0.13 | 30.1 | 32.9 | 37.0 |
190-1177A | 190-1177A-18R-1,19-24 | 74 | 13.0 | 18.4 | 5.4 | 0.0 | 1.6 | 13.6 | 6.6 | 33.2 | 2.2 | 0.2 | 0.2 | 0.0 | 2.6 | 5.0 | 0.0 | 0.2 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 100 | 1 | 0 | 38.5 | 20.2 | 41.3 | 12.7 | 6.3 | 81.0 | 0.18 | 0.67 | 0.06 | 39.2 | 19.9 | 41.0 |
190-1177A | 190-1177A-20R-2,78-82 | 76 | 11.6 | 27.4 | 6.6 | 0.0 | 1.6 | 19.8 | 10.4 | 15.6 | 3.4 | 0.0 | 0.2 | 0.0 | 3.6 | 2.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.8 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 2 | 47.6 | 30.4 | 22.0 | 11.9 | 16.5 | 71.6 | 0.17 | 0.66 | 0.17 | 27.8 | 24.9 | 47.4 |
190-1177A | 190-1177A-37R-3,148-150 | 732 | 20.4 | 31.2 | 3.6 | 0.0 | 2.0 | 13.8 | 14.0 | 5.2 | 7.4 | 0.2 | 0.4 | 0.0 | 8.0 | 1.2 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 100 | 1 | 0 | 57.4 | 27.9 | 14.7 | 8.3 | 55.6 | 36.1 | 0.10 | 0.50 | 0.55 | 42.3 | 29.0 | 28.6 |
190-1177A | 190-1177A-37R-4,9-12 | 733 | 17.8 | 39.0 | 7.0 | 0.0 | 2.8 | 16.0 | 5.4 | 8.4 | 2.2 | 0.2 | 0.2 | 0.0 | 2.6 | 0.8 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 0 | 4 | 66.6 | 21.4 | 12.0 | 6.8 | 22.0 | 71.2 | 0.15 | 0.75 | 0.22 | 45.4 | 13.8 | 40.8 |
190-1177A | 190-1177A-45R-1,84-88 | 745 | 15.8 | 28.8 | 5.2 | 0.0 | 4.2 | 14.2 | 20.2 | 4.0 | 6.0 | 0.2 | 0.2 | 0.0 | 6.4 | 1.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 0 | 3 | 54.1 | 34.5 | 11.4 | 8.8 | 56.1 | 35.1 | 0.17 | 0.41 | 0.56 | 31.5 | 40.2 | 28.3 |
190-1178A | 190-1178A-30X-5,76-81 | 817 | 12.4 | 12.6 | 3.8 | 0.0 | 2.2 | 7.4 | 7.6 | 51.2 | 0.6 | 0.2 | 0.0 | 0.0 | 0.8 | 1.0 | 0.4 | 0.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 2 | 0 | 31.0 | 15.0 | 54.0 | 3.7 | 1.5 | 94.8 | 0.19 | 0.49 | 0.01 | 45.3 | 27.7 | 27.0 |
190-1178A | 190-1178A-34X-1,128-132 | 820 | 14.6 | 10.4 | 3.4 | 0.2 | 2.6 | 7.6 | 10.8 | 47.8 | 0.4 | 0.4 | 0.0 | 0.0 | 0.8 | 1.0 | 0.0 | 0.8 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 2 | 2 | 31.2 | 18.4 | 50.4 | 3.6 | 1.6 | 94.8 | 0.19 | 0.41 | 0.02 | 44.2 | 32.7 | 23.0 |
190-1178A | 190-1178A-42X-1,125-139 | 828 | 13.2 | 8.8 | 3.0 | 0.2 | 2.4 | 6.0 | 9.2 | 54.6 | 2.0 | 0.0 | 0.0 | 0.0 | 2.0 | 0.4 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 2 | 4 | 27.6 | 15.2 | 57.2 | 1.0 | 3.5 | 95.5 | 0.20 | 0.39 | 0.03 | 46.5 | 32.4 | 21.1 |
190-1178A | 190-1178A-43X-3,34-40 | 831 | 11.6 | 8.4 | 4.6 | 0.0 | 4.6 | 4.8 | 4.6 | 57.6 | 1.6 | 0.2 | 0.0 | 0.0 | 1.8 | 1.4 | 0.0 | 0.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 1 | 29.2 | 9.4 | 61.4 | 3.3 | 2.9 | 93.8 | 0.32 | 0.51 | 0.03 | 55.2 | 21.9 | 22.9 |
190-1178B | 190-1178B-11R-4,36-39 | 838 | 11.0 | 10.8 | 3.2 | 0.0 | 1.0 | 7.8 | 5.4 | 59.4 | 0.2 | 0.0 | 0.0 | 0.0 | 0.2 | 0.2 | 0.0 | 0.8 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 4 | 26.1 | 13.2 | 60.7 | 1.7 | 0.3 | 98.0 | 0.16 | 0.59 | 0.00 | 45.5 | 22.3 | 32.2 |
190-1178B | 190-1178B-12R-2,32-33 | 839 | 11.8 | 13.6 | 5.2 | 0.0 | 3.8 | 10.6 | 10.6 | 41.4 | 1.4 | 0.2 | 0.0 | 0.0 | 1.6 | 0.8 | 0.0 | 0.2 | 0.0 | 0.0 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 0 | 3 | 34.5 | 21.3 | 44.2 | 2.3 | 3.6 | 94.1 | 0.26 | 0.50 | 0.04 | 35.8 | 32.1 | 32.1 |
190-1178B | 190-1178B-21R-2,66-71 | 846 | 12.6 | 11.6 | 8.2 | 0.0 | 4.0 | 9.2 | 10.0 | 40.6 | 2.0 | 0.0 | 0.0 | 0.0 | 2.0 | 1.6 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 2 | 7 | 36.4 | 19.2 | 44.4 | 4.1 | 4.5 | 91.4 | 0.34 | 0.48 | 0.05 | 39.6 | 31.4 | 28.9 |
190-1178B | 190-1178B-23R-2,45-47 | 848 | 7.0 | 9.8 | 3.4 | 0.0 | 2.6 | 10.8 | 10.2 | 47.2 | 4.0 | 0.0 | 0.0 | 0.0 | 4.0 | 3.6 | 0.0 | 0.4 | 0.8 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 6 | 22.8 | 21.0 | 56.1 | 7.2 | 7.2 | 85.5 | 0.26 | 0.51 | 0.07 | 25.0 | 36.4 | 38.6 |
190-1178B | 190-1178B-23R-2,133-135 | 849 | 6.6 | 13.0 | 4.6 | 0.0 | 3.8 | 8.8 | 4.8 | 53.2 | 2.6 | 0.2 | 0.0 | 0.0 | 2.8 | 2.0 | 0.0 | 0.2 | 0.2 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 2 | 2 | 28.0 | 13.6 | 58.4 | 3.8 | 4.8 | 91.4 | 0.30 | 0.65 | 0.05 | 32.7 | 23.8 | 43.6 |
190-1178B | 190-1178B-25R-2,51-53 | 852 | 7.0 | 12.2 | 4.4 | 0.0 | 1.4 | 10.0 | 6.0 | 51.6 | 4.8 | 0.6 | 0.0 | 0.0 | 5.4 | 1.4 | 0.2 | 0.4 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 4 | 25.0 | 16.0 | 59.0 | 3.4 | 9.2 | 87.5 | 0.23 | 0.63 | 0.09 | 30.4 | 26.1 | 43.5 |
190-1178B | 190-1178B-30R-3,15-20 | 856 | 6.4 | 18.2 | 4.0 | 0.0 | 3.6 | 9.8 | 6.4 | 48.4 | 1.6 | 0.0 | 0.0 | 0.0 | 1.6 | 1.6 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 0.0 | 100 | 1 | 2 | 32.2 | 16.2 | 51.6 | 3.1 | 3.1 | 93.8 | 0.24 | 0.60 | 0.03 | 28.3 | 28.3 | 43.4 |