Polyak, Boris G (2000): (Table 1) Isotopic and geochemical parameters of gas phase from underground fluids of the Baikal rift and its framing [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.744945
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Abstract:
Results of studying isotopic composition of helium in underground fluids of the Baikal-Mongolian region during the last quarter of XX century are summarized. Determinations of 3He/4He ratio in 139 samples of gas phase from fluids, collected at 104 points of the Baikal rift zone and adjacent structures are given. 3He/4He values lie within the range from 1x10**-8 (typical for crustal radiogenic helium) to 1.1x10**-5 (close to typical MORB reservoir). Repeated sampling in some points during more than 20 years showed stability of helium isotopic composition in time in each of them at any level of 3He/4He values. There is no systematic differences of 3He/4He in samples from surface water sources and deeper intervals of boreholes in the same areas. Universal relationship between isotopic composition of helium and general composition of gas phase is absent either, but the minimum 3He/4He values occurred in methane gas of hydrocarbon deposits, whereas in nitrogen and carbon dioxide gases of helium composition varied (in the latter maximum 3He/4He values have been measured). According to N2/Ar_atm ratio nitrogen gases are atmospheric. In carbonic gas fN2/fNe ratio indicates presence of excessive (non-atmogenic) nitrogen, but the attitude CO2/3He differs from one in MORB. Comparison of helium isotopic composition with its concentration and composition of the main components of gas phase from fluids shows that it is formed under influence of fractionation of components with different solubility in the gas-water system and generation/consumption of reactive gases in the crust. Structural and tectonic elements of the region differ from the spectrum of 3He/4He values. At the pre-Riphean Siberian Platform the mean 3He/4He = (3.6+/-0.9)x10**- 8 is very close to radiogenic one. In the Paleozoic crust of Khangay 3He/4He = (16.3+/-4.6)x10**-8, and the most probable estimate is (12.3+/-2.9)x10**-8. In structures of the eastern flank of the Baikal rift zone (Khentei, Dauria) affected by the Mz-Kz activization 3He/4He values range from 4.4x10**-8 to 2.14x10**-6 (average 0.94x10**-6). Distribution of 3He/4He values across the strike of the Baikal rift zone indicates advective heat transfer from the mantle not only in the rift zone, but also much further to the east. In fluids of the Baikal rift zone range of 3He/4He values is the widest: from 4x10**-8 to 1.1x10**-5. Their variations along the strike of the rift zone are clearly patterned, namely, decrease of 3He/4He values in both directions from the Tunka depression. Accompanied by decrease in density of conductive heat flow and in size of rift basins, this trend indicates decrease in intensity of advective heat transfer from the mantle to peripheral segments of the rift zone. Comparing this trend with data on other continental rift zones and mid-ocean ridges leads to the conclusion about fundamental differences in mechanisms of interaction between the crust and the mantle in these environments.
Related to:
Polyak, Boris G (2000): Helium isotopes in the Baikal rift underground fluids and its framing (to geodynamics of continental rift genesis). Russian Journal of Earth Sciences, 2(2), 109-133, https://doi.org/10.2205/2000ES000036
Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 52.220095 * Median Longitude: 106.310715 * South-bound Latitude: 45.733300 * West-bound Longitude: 97.566700 * North-bound Latitude: 58.866700 * East-bound Longitude: 118.466700
Minimum DEPTH, sediment/rock: -3150 m * Maximum DEPTH, sediment/rock: 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 | Area/locality | Area | Polyak, Boris G | |||
5 | Sample position | Samp pos | Polyak, Boris G | |||
6 | Sampling date | Sampling date | Polyak, Boris G | |||
7 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
8 | Temperature, water | Temp | °C | Polyak, Boris G | ||
9 | Temperature, water | Temp | °C | Polyak, Boris G | min | |
10 | Temperature, water | Temp | °C | Polyak, Boris G | max | |
11 | Helium | He | ppmv | Polyak, Boris G | Isotope ratio mass spectrometry | |
12 | Helium | He | ppmv | Polyak, Boris G | Isotope ratio mass spectrometry | +Ne |
13 | Neon | Ne | ppmv | Polyak, Boris G | Isotope ratio mass spectrometry | |
14 | Argon | Ar | ppmv | Polyak, Boris G | Isotope ratio mass spectrometry | |
15 | Helium-3/Helium-4 | 3He/4He | 10-4 | Polyak, Boris G | Isotope ratio mass spectrometry | corrected |
16 | Ratio | Ratio | Polyak, Boris G | Calculated | He/Ne | |
17 | Helium-4/Neon-20 | 4He/20Ne | Polyak, Boris G | Isotope ratio mass spectrometry | ||
18 | Argon-40/Argon-36 | 40Ar/36Ar | Polyak, Boris G | Isotope ratio mass spectrometry | ||
19 | Gas type | Gas typ | Polyak, Boris G |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
933 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Area | 5 Samp pos | 6 Sampling date | 7 Depth sed [m] | 8 Temp [°C] | 9 Temp [°C] (min) | 10 Temp [°C] (max) | 11 He [ppmv] (Isotope ratio mass spectrometry) | 12 He [ppmv] (+Ne, Isotope ratio mass spect...) | 13 Ne [ppmv] (Isotope ratio mass spectrometry) | 14 Ar [ppmv] (Isotope ratio mass spectrometry) | 15 3He/4He [10-4] (corrected, Isotope ratio mass...) | 16 Ratio (He/Ne, Calculated) | 17 4He/20Ne (Isotope ratio mass spectrometry) | 18 40Ar/36Ar (Isotope ratio mass spectrometry) | 19 Gas typ |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Polyak-2000-1 | 53.92 | 104.55 | SIBERIAN PLATFORM, Irkutsk amphitheater | Khristoforovskaya site, hole 12 | <1976 | -1150 | 480 | 2000.00 | 0.00042 | CH4 | ||||||||
Polyak-2000-2 | 55.13 | 105.22 | Irkutsk amphitheater | Gruznovskaya site | <1976 | -2680 | 2500 | 440.00 | 0.00010 | CH4 | ||||||||
Polyak-2000-3 | 53.83 | 103.83 | Irkutsk amphitheater | Shamanovskaya site | <1976 | -2460 | 2800 | 460.00 | 0.00018 | CH4 | ||||||||
Polyak-2000-4 | 53.52 | 103.65 | Irkutsk amphitheater | Bil´chrskaya site | <1976 | -2280 | 1920 | 390.00 | 0.00025 | (CH4) | ||||||||
Polyak-2000-5 | 53.67 | 102.77 | Irkutsk amphitheater | Novo-Nukutskaya site | <1976 | -450 | 790 | 1500.00 | 0.00059 | (CH4) | ||||||||
Polyak-2000-6 | 53.72 | 102.83 | Irkutsk amphitheater | Nukutskaya site | <1976 | -430 | 170 | 11000.00 | 0.00030 | N2 | ||||||||
Polyak-2000-7 | 53.37 | 103.98 | Irkutsk amphitheater | Osinskaya site, hole R-1 | <1976 | -1650 | 13.0 | 530 | 990.00 | 0.00035 | (CH4) | |||||||
Polyak-2000-8 | 53.28 | 104.10 | Irkutsk amphitheater | Parfenovskaya site, hole R-3 | <1976 | -2400 | 35.0 | 2460 | 960.00 | 0.00023 | (CH4) | |||||||
Polyak-2000-9 | 52.30 | 104.25 | Irkutsk amphitheater | Angara resort, hole 223 | 1995 | -982 | 15.0 | 2011 | 19.80 | 13710.00 | 0.00037 | 110.500 | 297.7 | N2 | ||||
Polyak-2000-10 | 52.30 | 104.25 | Irkutsk amphitheater | Angara resort, hole 110 | <1976 | -700 | 16.0 | 990 | 15800.00 | 0.00040 | N2 | |||||||
Polyak-2000-11 | 52.62 | 103.83 | Irkutsk amphitheater | Angarsk hole | <1976 | -400 | 740 | 12500.00 | 0.00043 | (N2) | ||||||||
Polyak-2000-12 | 52.40 | 104.15 | Irkutsk amphitheater | Batareinaya st. | <1976 | -400 | 320 | 10700.00 | 0.00055 | (N2) | ||||||||
Polyak-2000-13 | 53.08 | 105.50 | Irkutsk amphitheater | Bayanday village | <1976 | -118 | 770 | 20800.00 | 0.00100 | (N2) | ||||||||
Polyak-2000-14 | 53.08 | 102.37 | Irkutsk amphitheater | Golumet´ village | <1976 | -60 | 310 | 20000.00 | 0.00050 | (N2) | ||||||||
Polyak-2000-15 | 56.55 | 102.27 | Nepsky arch | Bratskaya site | <1976 | -3020 | 2000.0 | 0.00065 | (CH4) | |||||||||
Polyak-2000-16 | 57.22 | 106.47 | Nepsky arch | Kosatkinskaya site | <1976 | -2760 | 7500.0 | 0.00012 | (CH4) | |||||||||
Polyak-2000-17 | 58.17 | 106.23 | Nepsky arch | Nepskaya site | <1976 | -2600 | 1960.0 | 0.00016 | (CH4) | |||||||||
Polyak-2000-18 | 58.17 | 105.88 | Nepsky arch | Verkhne-Nepskaya site | <1976 | -1300 | 1550.0 | 0.00016 | (CH4) | |||||||||
Polyak-2000-19 | 57.77 | 107.07 | Nepsky arch | Severo-Markovskaya site | <1976 | -2600 | 280.0 | 0.00012 | (CH4) | |||||||||
Polyak-2000-20 | 57.77 | 107.07 | Nepsky arch | Severo-Markovskaya site | <1976 | -2200 | 3300.0 | 0.00100 | (CH4) | |||||||||
Polyak-2000-21 | 57.92 | 107.13 | Nepsky arch | Yaraktinskaya site | <1976 | -2700 | 950.0 | 266.00 | 0.00020 | 1673.0 | (CH4) | |||||||
Polyak-2000-22 | 56.03 | 103.28 | Nepsky arch | Yuzhnaya site | <1976 | -3150 | 1540.0 | 0.00022 | (CH4) | |||||||||
Polyak-2000-23 | 58.87 | 102.65 | Nepsky arch | Endarma village | <1976 | 600.0 | 0.00020 | |||||||||||
Polyak-2000-24 | 58.50 | 107.00 | Nepsky arch | 2.5 km from the Usa river mouth | <1976 | 0 | 350.0 | 0.00025 | ||||||||||
Polyak-2000-25 | 54.03 | 100.00 | Nepsky arch | Karasaiskaya site | <1976 | -1180 | 4250.0 | 0.00120 | ||||||||||
Polyak-2000-26 | 58.05 | 109.47 | Nepsky arch | Lena river, 4.5 km from the Chai river mouth | <1976 | 0 | 310.0 | 0.00025 | ||||||||||
Polyak-2000-27 | 58.25 | 108.00 | Nepsky arch | Nepa riv, spring 1 | <1976 | 0 | 27000.0 | 0.00100 | ||||||||||
Polyak-2000-28 | 58.25 | 108.00 | Nepsky arch | Nepa riv, spring 2 | <1976 | 0 | 300.0 | 0.00052 | ||||||||||
Polyak-2000-29 | 58.25 | 107.00 | Nepsky arch | Zenan river, headwater | <1976 | 0 | 2100.0 | 0.00025 | ||||||||||
Polyak-2000-30 | 56.90 | 118.25 | BAIKAL KHUBSUGUL RIFT ZONE, Upper Charskaya depression | Verhne-Charsky spring, bath 2 | 1984 | 0 | 14200 | 12000.00 | 0.00098 | N2 | ||||||||
Polyak-2000-31 | 56.85 | 118.20 | Upper Charskaya depression | Luktur spring | 1984 | 0 | 42.0 | 22000 | 16000.00 | 0.00049 | (N2) | |||||||
Polyak-2000-32 | 56.25 | 116.88 | Udokan ridge | Plotinny spring | <1995 | 0 | 0.00050 | (N2) | ||||||||||
Polyak-2000-33 | 56.25 | 117.05 | Udokan ridge | Travertinovy spring | <1995 | 0 | 0.00170 | (N2) | ||||||||||
Polyak-2000-34 | 56.27 | 113.63 | North Muisky ridge | Itykitsky spring | <1995 | 0 | 0.00180 | (N2) | ||||||||||
Polyak-2000-35 | 56.18 | 113.58 | North Muisky ridge | Severo-Muisky spring (tunnel galery) | <1995 | 0.00180 | (N2) | |||||||||||
Polyak-2000-36 | 56.10 | 113.68 | North Muisky ridge | Okusikansky spring | <1995 | 0 | 0.00080 | (N2) | ||||||||||
Polyak-2000-37 | 55.95 | 110.55 | Verkhne Angarsk depression | Dzhelinda spring | <1995 | 0 | 0.00180 | (N2) | ||||||||||
Polyak-2000-38 | 55.85 | 111.20 | Verkhne Angarsk depression | Irkana spring | 1984 | 0 | 2450.0 | 9.66 | 0.00500 | 279.000 | 301.0 | (N2) | ||||||
Polyak-2000-39 | 54.37 | 109.52 | North Baikal depression | Davshinsky spring | 1975 | 0 | 45.0 | 190 | 17000.00 | 0.00450 | N2 | |||||||
Polyak-2000-40 | 55.50 | 109.95 | North Baikal depression | Frolihinsky spring | 1975 | 0 | 36.0 | 780 | 14200.00 | 0.00150 | N2 | |||||||
Polyak-2000-41 | 55.40 | 109.95 | North Baikal depression | Khakussky spring | 1975 | 0 | 46.0 | 720 | 12000.00 | 0.00190 | N2 | |||||||
Polyak-2000-42 | 55.40 | 109.95 | North Baikal depression | Khakussky spring | 1994 | 0 | 46.0 | 0.00180 | 47.060 | N2 | ||||||||
Polyak-2000-43 | 55.05 | 109.07 | North Baikal depression | Kotel´nikovsky spring | 1975 | 0 | 64.0 | 4100 | 17800.00 | 0.00050 | N2 | |||||||
Polyak-2000-44 | 53.67 | 108.98 | North Baikal depression | Kulinykh swamp spring | 1975 | 0 | 26.0 | 100 | 17600.00 | 0.00180 | N2 | |||||||
Polyak-2000-45 | 53.75 | 109.00 | North Baikal depression | Zmeiny spring | 1975 | 0 | 46.0 | 500 | 14000.00 | 0.00400 | N2 | |||||||
Polyak-2000-46 | 53.62 | 109.37 | North Baikal depression | Gniloi spring | <1995 | 0 | 0.00720 | (N2) | ||||||||||
Polyak-2000-47 | 55.70 | 109.08 | North Baikal depression | Solnechny spring | <1995 | 0 | 0.00080 | (N2) | ||||||||||
Polyak-2000-48 | 52.97 | 108.30 | Middle Baikal depression | Goryachinsky spring | 1972 | 0 | 54.0 | 820 | 0.00410 | (N2) | ||||||||
Polyak-2000-49 | 52.97 | 108.30 | Middle Baikal depression | Goryachinsky spring | 1975 | 0 | 54.0 | 750 | 0.00420 | (N2) | ||||||||
Polyak-2000-50 | 52.97 | 108.30 | Middle Baikal depression | Goryachinsky spring | 1976 | 0 | 629 | 0.00550 | (N2) | |||||||||
Polyak-2000-51 | 52.97 | 108.30 | Middle Baikal depression | Goryachinsky spring | 1984 | 0 | 54.0 | 1050 | 10500.00 | 0.00560 | (N2) | |||||||
Polyak-2000-52 | 52.52 | 107.23 | Middle Baikal depression | Sukhaya Zagza site | 1975 | 27.0 | 290 | 0.00450 | (N2) | |||||||||
Polyak-2000-53 | 52.52 | 107.23 | Middle Baikal depression | Sukhaya Zagza site | 1984 | 27.0 | 320 | 1900.00 | 0.00850 | (N2) | ||||||||
Polyak-2000-54 | 52.52 | 107.23 | Middle Baikal depression | Sukhaya Zagza site | 0.01000 | (N2) | ||||||||||||
Polyak-2000-55 | 51.70 | 105.83 | South Baikal depression | Svyatoy Klyuch spring | 0 | 0.03000 | (N2) | |||||||||||
Polyak-2000-56 | 51.62 | 102.38 | Tungus depression | Zhemchug site, hole R-1 | 1973 | -796 | 38.0 | 2420.0 | 3108.00 | 0.11200 | 410.0 | CH4 | ||||||
Polyak-2000-57 | 51.62 | 102.38 | Tungus depression | Zhemchug site, hole R-1 | 1985 | 38.0 | 2600.0 | 2400.00 | >0.08500 | CH4 | ||||||||
Polyak-2000-58 | 51.62 | 102.38 | Tungus depression | Zhemchug site, hole G-1 | 1995 | 54.0 | 430.0 | 0.64 | 809.00 | 0.08000 | 742.000 | 322.5 | CO2 | |||||
Polyak-2000-59 | 51.62 | 102.38 | Tungus depression | Zhemchug site, hole 2 | <1995 | 0.06200 | ||||||||||||
Polyak-2000-60 | 51.62 | 102.38 | Tungus depression | Zhemchug site, hole 1 | <1995 | 0.07450 | ||||||||||||
Polyak-2000-61 | 51.90 | 102.47 | Tungus depression | Arshan resort, Glaznoy spring | 1975 | 0 | 8.0 | 210 | 2300.00 | 0.11000 | CO2 | |||||||
Polyak-2000-62 | 51.90 | 102.47 | Tungus depression | Arshan resort, Glaznoy spring | 1983 | 0 | 8.0 | 506.0 | 3.43 | 0.08600 | 162.000 | 303.0 | CO2 | |||||
Polyak-2000-63 | 51.90 | 102.47 | Tungus depression | Arshan resort, Glaznoy spring | 1995 | 0 | 9.5 | 1176.0 | 4.10 | 4010.00 | 0.09940 | 315.000 | 307.5 | CO2 | ||||
Polyak-2000-64 | 51.90 | 102.47 | Tungus depression | Arshan resort, hole 26 | 1973 | -490 | 21.0 | 50.0 | 4213.00 | 0.09500 | 315.0 | CO2 | ||||||
Polyak-2000-65 | 51.90 | 102.47 | Tungus depression | Arshan resort, hole 28 | 1985 | 43.0 | 14 | 770.00 | 0.10000 | CO2 | ||||||||
Polyak-2000-66 | 51.90 | 102.47 | Tungus depression | Arshan resort, hole 39 | 1995 | -750 | 43.0 | 80.4 | 0.15 | 180.00 | 0.09835 | 614.500 | 315.6 | CO2 | ||||
Polyak-2000-67 | 51.68 | 101.68 | Tungus depression | Nilova Pustyn´ resort, hole | <1995 | 0.02140 | N2 | |||||||||||
Polyak-2000-68 | 51.68 | 101.68 | Tungus depression | Nilova Pustyn´ resort, hole 1 | 1973 | 41.0 | 30.0 | 10033.00 | 0.02800 | 300.0 | N2 | |||||||
Polyak-2000-69 | 50.78 | 100.80 | Khubsugul depression | Bulnai spring | 1982 | 0 | 47.0 | 5740.0 | 0.00460 | N2 | ||||||||
Polyak-2000-70 | 50.78 | 100.80 | Khubsugul depression | Bulnai spring | 27.07.1987 | 0 | 49.5 | 0.00460 | (N2) | |||||||||
Polyak-2000-71 | 51.33 | 101.00 | Khubsugul depression | Chzhilge spring | 1982 | 0 | 6.0 | 23.0 | 19.40 | 0.00300 | 1.270 | 296.0 | N2 | |||||
Polyak-2000-72 | 51.54 | 100.42 | Khubsugul depression | Delger-Bulag spring | 1982 | 0 | 4.0 | 90.0 | 19.30 | 0.00560 | 5.040 | 296.0 | N2 | |||||
Polyak-2000-73 | 49.42 | 100.29 | Khubsugul depression | Naran-Bulag spring | 1988 | 0 | 0.2 | 9.0 | 19.20 | 0.00500 | 0.500 | 300.0 | N2 | |||||
Polyak-2000-74 | 51.55 | 100.80 | Khubsugul depression | Oboni spring | 1982 | 0 | 3.0 | 9.0 | 18.90 | 0.01420 | 0.496 | 296.0 | N2 | |||||
Polyak-2000-75 | 51.61 | 100.60 | Khubsugul depression | Bilyutyin spring | 1982 | 0 | 5.0 | 180.0 | 23.00 | 0.00740 | 7.8 | (N2) | ||||||
Polyak-2000-76 | 50.07 | 100.05 | Khubsugul depression | Ulkhen spring | 07.1973 | 0 | 2.8 | 140.0 | 0.02900 | |||||||||
Polyak-2000-77 | 50.07 | 100.05 | Khubsugul depression | Ulkhen spring | 1982 | 0 | 2.8 | 22.00 | 0.02960 | 6.4 | ||||||||
Polyak-2000-78 | 54.70 | 110.70 | Barguzin depression | Allinsky spring | 0 | 0.00810 | N2 | |||||||||||
Polyak-2000-79 | 53.43 | 109.42 | Barguzin depression | Gusikhinsky spring | <1976 | 0 | 55.0 | 1500 | 15600.00 | 0.00610 | N2 | |||||||
Polyak-2000-80 | 54.98 | 111.12 | Barguzin depression | Umheisky spring | <1976 | 0 | 46.0 | 1200 | 12000.00 | 0.00300 | N2 | |||||||
Polyak-2000-81 | 55.12 | 112.98 | Bauntovskaya depression | Bauntovsky spring | <1976 | 0 | 48.0 | 15000.00 | 0.00340 | N2 | ||||||||
Polyak-2000-82 | 55.12 | 112.98 | Bauntovskaya depression | Bauntovsk spring | 0 | 0.00250 | N2 | |||||||||||
Polyak-2000-83 | 55.37 | 113.50 | Bauntovskaya depression | Busansky spring | <1976 | 0 | 53.0 | 4300 | 14000.00 | 0.00160 | N2 | |||||||
Polyak-2000-84 | 55.52 | 113.83 | Bauntovskaya depression | Frantsevo spring | 0 | 0.00340 | (N2) | |||||||||||
Polyak-2000-85 | 55.42 | 113.58 | Bauntovskaya depression | Mogoisky spring | 0 | 0.00250 | (N2) | |||||||||||
Polyak-2000-86 | 50.32 | 110.97 | TRANSBAIKALIA (DAURIA) | Angi-Arshan spring | 1995 | 0 | 3.0 | 3720.0 | 9.90 | 6970.00 | 0.00044 | 412.000 | 298.3 | CH4 | ||||
Polyak-2000-87 | 51.18 | 113.80 | Transbaikalia (Dauria) | Darasun resort, hole 6/56 | 1984 | 2.4 | 320.0 | 500.00 | 0.00790 | CO2 | ||||||||
Polyak-2000-88 | 50.70 | 110.97 | Transbaikalia (Dauria) | Kapchagir spring | 1995 | 0 | 3.5 | 47.0 | 1.70 | 2.28 | 0.02060 | 31.000 | 299.5 | CO2 | ||||
Polyak-2000-89 | 51.75 | 112.97 | Transbaikalia (Dauria) | Kuka resort, hole 41 | 1972 | 0.2 | 190.0 | 0.01850 | CO2 | |||||||||
Polyak-2000-90 | 50.65 | 110.07 | Transbaikalia (Dauria) | Moduy spring | 1995 | 0 | 4.0 | 21.0 | 0.33 | 461.00 | 0.01870 | 69.000 | 303.5 | CO2 | ||||
Polyak-2000-91 | 50.63 | 110.48 | Transbaikalia (Dauria) | Poperechny spring | 1995 | 0 | 4.0 | 22.0 | 0.20 | 334.00 | 0.02140 | 119.000 | 305.4 | CO2 | ||||
Polyak-2000-92 | 51.83 | 116.67 | Transbaikalia (Dauria) | Urguchan resort | 1970 | 2.0 | 0.01100 | CO2 | ||||||||||
Polyak-2000-93 | 50.63 | 110.25 | Transbaikalia (Dauria) | Yamarovka resort | 1972 | 180 | 0.00500 | CO2 | ||||||||||
Polyak-2000-94 | 50.63 | 110.25 | Transbaikalia (Dauria) | Yamarovka resort, hole 15 | 1995 | 4.0 | 45.0 | 0.20 | 195.00 | 0.00950 | 244.000 | 305.7 | CO2 | |||||
Polyak-2000-95 | 50.57 | 110.90 | Transbaikalia (Dauria) | Mergitaika spring | 1995 | 0 | 5.0 | 0.3 | 0.10 | 111.00 | 0.01410 | 3.000 | 296.5 | (CO2) | ||||
Polyak-2000-96 | 50.25 | 110.07 | Transbaikalia (Dauria) | Kunaley spring | 1995 | 0 | 19.5 | 1029.0 | 21.00 | 11200.00 | 0.00074 | 54.000 | 295.7 | N2 | ||||
Polyak-2000-97 | 51.50 | 118.47 | Transbaikalia (Dauria) | Yamkun spring | 1984 | 0 | 17.5 | 1400 | 600.00 | 0.00470 | N2 | |||||||
Polyak-2000-98 | 47.33 | 110.07 | KHENTEI-KERULENSK ZONE | Dashi-Chigyn spring | 1983 | 0 | 10.0 | 230.0 | 2.56 | 0.01200 | 98.000 | 292.0 | CO2 | |||||
Polyak-2000-99 | 47.90 | 100.92 | Khentei-Kerulensk zone | Orgil spring | 1982 | 0 | 2 | 5 | <20.0 | 0.01100 | CO2 | |||||||
Polyak-2000-100 | 47.90 | 100.92 | Khentei-Kerulensk zone | Orgil spring | 06.04.1989 | 0 | 3.5 | 0.01100 | CO2 | |||||||||
Polyak-2000-101 | 47.56 | 109.40 | Khentei-Kerulensk zone | Urta spring | 1982 | 0 | 4.0 | <30.0 | 0.01900 | CO2 | ||||||||
Polyak-2000-102 | 47.56 | 109.40 | Khentei-Kerulensk zone | Urta spring | 21.08.1989 | 0 | 1.5 | 0.01900 | CO2 | |||||||||
Polyak-2000-103 | 46.19 | 109.35 | Khentei-Kerulensk zone | Dundyn-Amralt spring | 1982 | 0 | 10.0 | 2370.0 | 0.00130 | N2 | ||||||||
Polyak-2000-104 | 48.75 | 115.17 | Khentei-Kerulensk zone | Minzhur spring | 1988 | 0 | 60.0 | 7.0 | 19.20 | 0.00580 | 0.410 | 296.0 | N2 | |||||
Polyak-2000-105 | 47.83 | 110.10 | Khentei-Kerulensk zone | Yargach spring | 1982 | 0 | 1.0 | 240.0 | 24.00 | 0.00270 | 10.0 | N2 | ||||||
Polyak-2000-106 | 47.10 | 109.10 | Khentei-Kerulensk zone | Avrag spring | 24.06.1990 | 0 | 8.0 | 0.00650 | ||||||||||
Polyak-2000-107 | 47.05 | 112.73 | Khentei-Kerulensk zone | Tal-Bulag spring | 22.06.1990 | 0 | 3.4 | 0.01300 | ||||||||||
Polyak-2000-108 | 47.80 | 97.57 | KHANGAISK UPLAND | Bogdo-Ula spring | 1988 | 0 | 41 | 54 | 1200.0 | 13.30 | 0.00060 | 98.000 | 299.0 | N2 | ||||
Polyak-2000-109 | 46.75 | 100.43 | Khangaisk upland | Bor-Tal spring | 14.07.1990 | 0 | 46.5 | 0.00180 | (N2) | |||||||||
Polyak-2000-110 | 47.76 | 100.24 | Khangaisk upland | Chulutu spring | 1982 | 0 | 44.0 | 9700.0 | 0.00120 | N2 | ||||||||
Polyak-2000-111 | 47.76 | 100.24 | Khangaisk upland | Chulutu spring | 16.07.1989 | 0 | 45.0 | 0.00120 | N2 | |||||||||
Polyak-2000-112 | 47.08 | 101.00 | Khangaisk upland | G´yalgar spring | 15.07.1990 | 0 | 52.0 | 0.00210 | (N2) | |||||||||
Polyak-2000-113 | 47.40 | 101.60 | Khangaisk upland | Khalun-Us spring | 1982 | 0 | 86.0 | 5490.0 | 0.00260 | N2 | ||||||||
Polyak-2000-114 | 47.40 | 101.60 | Khangaisk upland | Khalun-Us spring | 11.08.1978 | 0 | 35.0 | 0.00260 | N2 | |||||||||
Polyak-2000-115 | 48.33 | 98.37 | Khangaisk upland | Khodzhulin spring | 1982 | 0 | 35.0 | 2400.0 | 0.00110 | N2 | ||||||||
Polyak-2000-116 | 48.33 | 98.37 | Khangaisk upland | Khodzhulin spring | 13.08.1978 | 0 | 45.0 | 0.00110 | N2 | |||||||||
Polyak-2000-117 | 46.90 | 102.77 | Khangaisk upland | Khudzhirte spring | 1982 | 0 | 44.0 | 7220.0 | 0.00130 | N2 | ||||||||
Polyak-2000-118 | 46.90 | 102.77 | Khangaisk upland | Khudzhirte spring | 16.04.1990 | 0 | 55.0 | 0.00110 | N2 | |||||||||
Polyak-2000-119 | 48.25 | 102.98 | Khangaisk upland | Khul´dzhi spring | 1983 | 0 | 51.0 | 3800.0 | 12.50 | 0.00340 | 333.000 | 299.0 | N2 | |||||
Polyak-2000-120 | 48.65 | 102.62 | Khangaisk upland | Khul´dzhi (Saikhan-Khul´dzh) spring | 23.06.1990 | 0 | 51 | 56 | 0.00300 | N2 | ||||||||
Polyak-2000-121 | 46.33 | 101.22 | Khangaisk upland | Shargalzhut spring | 1983 | 0 | 90.0 | 1740.0 | 14.50 | 0.00360 | 131.000 | 294.0 | N2 | |||||
Polyak-2000-122 | 47.65 | 101.53 | Khangaisk upland | Shibertu spring | 1982 | 0 | 60.0 | 3740.0 | 14.20 | 0.00097 | 290.000 | 301.0 | N2 | |||||
Polyak-2000-123 | 47.65 | 101.53 | Khangaisk upland | Shibertu spring | 16.07.1990 | 0 | 59.0 | 0.00084 | N2 | |||||||||
Polyak-2000-124 | 49.25 | 98.32 | Khangaisk upland | Toshint spring | 0 | 4.0 | 0.00420 | (N2) | ||||||||||
Polyak-2000-125 | 47.03 | 102.03 | Khangaisk upland | Tsagan-Sumeit spring | 12.07.1990 | 0 | 69.0 | 0.00140 | (N2) | |||||||||
Polyak-2000-126 | 47.22 | 99.60 | Khangaisk upland | Tsokhot spring | 1988 | 0 | 20.5 | 3170.0 | 15.30 | 0.00124 | 227.000 | 298.0 | N2 | |||||
Polyak-2000-127 | 48.35 | 98.78 | Khangaisk upland | Zartyn-Halun spring | 1982 | 0 | 38.0 | 1010.0 | 7.05 | 0.00049 | 158.000 | 297.0 | N2 | |||||
Polyak-2000-128 | 45.73 | 106.72 | GOBI | Ara-Shantu spring | 1983 | 0 | 10.0 | 252.0 | 6.60 | 0.00460 | 42.200 | 293.0 | CO2 |