Rashidov, V A; Nevretdinov, E B; Selyangin, O B; Nevretdinov, Er B (2003): (Table 2) Absolute age of Magellan Seamount Guyots [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.785124, Supplement to: Rashidov, VA et al. (2003): Geologic-geophysical investigations of Magellan Seamount Guyots, Pacific Ocean. Vestnik KRAUNC (Bulletin of Kamchanka Regional Association "Educational-Scientific Center"). Earth Sciences, No 1, 103-126
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Abstract:
This paper generalizes both original data and all available materials obtained by home and foreign researchers when studying guyots of the Magellan seamounts. The Magellan seamounts represent an extended arc-like chain of seamounts, mainly guyots within the middle part of the East-Mariana Trough. The guyots rise above the relatively flat floor of the East-Mariana Trough with depths about 5500-6000 m to the height up to 4500-4800 m and reach depth level from 1300 to 1200 m. In 1980s-1990s the Magellan seamounts become objects of permanent studies for both home and foreign researchers. First of all it is connected with the fact that considerable accumulations of Fe/Mn crusts and nodules were found at slopes and tops of the Magellan seamounts. Though having some similar features, the guyots of the Magellan seamounts differ considerably in their geological structure, time of formation and duration of volcanic activity. They were studied rather non-uniformly. The Ita-Maitai, Dalmorgeo, Roskomnedra, Vulkanolog, TIG, Hemler guyots and the Himu seamount were studied in detail, while the Nakhodka, IMGiG, TOI, DVGI guyots and the D-4 and Golden Dragonseamounts are less studied. The MA-3, MA-4, MA-10, MA-11, MA-27, MA-29, MA-31 and MA-38 guyots are very poorly studied.
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 16.777083 * Median Longitude: 154.400208 * South-bound Latitude: 12.970000 * West-bound Longitude: 151.566667 * North-bound Latitude: 21.700000 * East-bound Longitude: 156.750000
Minimum Elevation: -4500.0 m * Maximum Elevation: -1200.0 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Elevation of event 2 | Elevation 2 | m | |||
6 | Area/locality | Area | Rashidov, V A | |||
7 | Rock type | Rock | Rashidov, V A | |||
8 | Age, mineral | Age mineral | Ma | Rashidov, V A | ||
9 | Age, mineral | Age mineral | Ma | Rashidov, V A | min | |
10 | Age, mineral | Age mineral | Ma | Rashidov, V A | max | |
11 | Age, error | Age e | ± | Rashidov, V A | ||
12 | Number of observations | NOBS | # | Rashidov, V A | ||
13 | Age, mineral | Age mineral | Ma | Rashidov, V A | average | |
14 | Age, error | Age e | ± | Rashidov, V A | average | |
15 | Analytical method | Method | Rashidov, V A |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
244 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Elevation 2 [m] | 6 Area | 7 Rock | 8 Age mineral [Ma] | 9 Age mineral [Ma] (min) | 10 Age mineral [Ma] (max) | 11 Age e [±] | 12 NOBS [#] | 13 Age mineral [Ma] (average) | 14 Age e [±] (average) | 15 Method |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
RNSN-03-01 | 21.30 | 153.20 | Golden Dragon Seamount | ankaramite | 95.0 | 95.0 | Ar/Ar | |||||||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 121.0 | 0.8 | 121.0 | 0.8 | Ar/Ar | |||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 120.2 | 0.8 | 119.6 | 0.7 | Ar/Ar | |||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 120.5 | 2.6 | Ar/Ar | |||||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 120.2 | 1.0 | Ar/Ar | |||||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 117.3 | 1.0 | Ar/Ar | |||||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 120.5 | 0.9 | Ar/Ar | |||||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 118.4 | 1.3 | Ar/Ar | |||||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 119.3 | 0.8 | 119.5 | 0.8 | Ar/Ar | |||
RNSN-03-02 | 21.70 | 151.70 | -4500 | -3440 | Himu Seamount | alkali basalt | 119.6 | 0.8 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 98.8 | 0.7 | 99.5 | 0.6 | Ar/Ar | |||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 100.4 | 0.7 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 100.1 | 0.8 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 99.4 | 0.8 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 99.1 | 0.9 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 99.4 | 1.0 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 99.5 | 1.3 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 100.4 | 1.5 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 99.6 | 0.9 | 100.7 | 0.6 | Ar/Ar | |||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 102.2 | 1.3 | Ar/Ar | |||||
RNSN-03-03 | 19.55 | 151.57 | -3950 | -2510 | Hemler Guyot | alkali basalt | 101.0 | 0.9 | Ar/Ar | |||||
RNSN-03-04 | 19.50 | 153.60 | D-4 Seamount | alkali basalt | 74.0 | 74.0 | Ar/Ar | |||||||
RNSN-03-05 | 17.20 | 154.30 | -2200 | Dalmorgeo Guyot, main edifice | hawaiite | 92.3 | 1.7 | 94.8 | 1.2 | Ar/Ar | ||||
RNSN-03-05 | 17.20 | 154.30 | -2200 | Dalmorgeo Guyot, main edifice | hawaiite | 95.0 | 0.7 | Ar/Ar | ||||||
RNSN-03-05 | 17.20 | 154.30 | -2200 | Dalmorgeo Guyot, main edifice | hawaiite | 95.4 | 1.5 | Ar/Ar | ||||||
RNSN-03-05 | 17.20 | 154.30 | -2200 | Dalmorgeo Guyot, main edifice | alkali basalt | 96.6 | 0.7 | Ar/Ar | ||||||
RNSN-03-06 | 16.40 | 154.35 | -3400 | Oma Vlinder Guyot | hawaiite | 95.6 | 0.7 | 94.5 | 1.5 | Ar/Ar | ||||
RNSN-03-06 | 16.40 | 154.35 | -3400 | Oma Vlinder Guyot | hawaiite | 93.3 | 2.2 | Ar/Ar | ||||||
RNSN-03-07 | 17.03 | 154.07 | -2400 | Oma Vlinder Guyot, NW part | basanite | 100.2 | 0.4 | 102.2 | 0.4 | Ar/Ar | ||||
RNSN-03-08 | 16.98 | 154.02 | -3100 | Oma Vlinder Guyot | basanite | 102.4 | 0.5 | 102.0 | 0.6 | Ar/Ar | ||||
RNSN-03-08 | 16.98 | 154.02 | -3100 | Oma Vlinder Guyot | basanite | 101.6 | 0.6 | Ar/Ar | ||||||
RNSN-03-09 | 16.57 | 154.43 | -1200 | Oma Vlinder Guyot, summit plateau | basanite | 15.0 | 2.0 | 15.0 | 2.0 | K-Ar | ||||
RNSN-03-09a | 16.57 | 154.43 | -1200 | -3500 | Oma Vlinder Guyot, main edifice | trachyandesite, plagiobasalt | 36 | 95 | 15 | 63.0 | K-Ar | |||
RNSN-03-10 | 15.88 | 155.15 | -2025 | Nakhodka Guyot | hawaiite | 90.9 | 0.5 | 90.9 | 0.5 | Ar/Ar | ||||
RNSN-03-11 | 15.50 | 155.02 | -1600 | Nakhodka Guyot | hawaiite | 91.2 | 0.4 | 91.8 | 0.6 | Ar/Ar | ||||
RNSN-03-11 | 15.50 | 155.02 | -1600 | Nakhodka Guyot | hawaiite | 92.3 | 0.7 | Ar/Ar | ||||||
RNSN-03-12 | 14.13 | 155.15 | -4000 | IOAN Guyot | hawaiite | 88.5 | 0.7 | 88.5 | 0.7 | Ar/Ar | ||||
RNSN-03-13 | 14.18 | 155.98 | -1600 | IOAN Guyot | hawaiite | 86.7 | 0.4 | 86.7 | 0.4 | Ar/Ar | ||||
RNSN-03-14 | 12.98 | 156.68 | -4000 | Ita-Maitai Guyot | hawaiite | 120.0 | 0.8 | 120.0 | 0.9 | Ar/Ar | ||||
RNSN-03-14 | 12.98 | 156.68 | -4000 | Ita-Maitai Guyot | hawaiite | 117.9 | 0.9 | Ar/Ar | ||||||
RNSN-03-15 | 12.97 | 156.75 | -2700 | Ita-Maitai Guyot | hawaiite | 118.5 | 0.8 | 118.3 | 0.8 | Ar/Ar | ||||
RNSN-03-15 | 12.97 | 156.75 | -2700 | Ita-Maitai Guyot | hawaiite | 118.0 | 0.7 | Ar/Ar |