L-47
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(1)
Geological map
of Mongolia (1:1,000,000 in scale)
MRAM
Geological Survey and MAS Institute of Geology and Mineral Resources (1998)
Long.,
Lat.: (96 00, 44 00), (102 00, 44 00), (96 00, 48 00), (102 00, 48 00)
--- L-47 map (png)
--- Legend (png)
Please use two windows; one is for geological map,
the other is for legend. New window
can be opened by gCtrlh + gNh.
(2) (3) (4) Geology of the Bayankhongol
area, Mongolia (Scale 1:200,000)
Explanation
Text
(2) Geologic map (L47-9) (98 00-99 00 E, N 46
40-47 20 N)
(2) Geologic map (L-47-10) (99 00-100 00 E, 46
40-47 20 N)
(3) Geologic map (L-47-16) (99 00-100 00 E, 46
00-46 40 N)
(3) Geologic map (L-47-17) (100 00-101 00 E, 46
00-46 40 N)
(4) Geologic map (L-47-24) (101 00-102 00 E, 45
20-46 00 N)
(4) Geologic map (L-47-23) (100 00-101 00 E, 45
20-46 00 N)
(5)
Sereenen
JARGALAN and Satoshi MURAO (1998) Preliminary study on the characteristics of
Tsagaan tsakhir uul gold
deposit, Bayankhongor, southern Mongolia. Bull. GSJ, vol. 49 (6), p. 291-298. (Detail map near 46 40 N and 100 00 E is
shown in Fig.2),
(6)
Javkhlan et al.
(2013) Metamorphic pressure-temperature evolution of garnet-chloritoid schists
from the Lake Zone, SW Mongolia.
JMPS, vol. 108 (5), p. 255-266.
(Detail map around 45 20 N and 98 12 E is shown in Fig. 2).
(8) Bayasgalan, T., Munkhtsengel,
B., Khishigsuren, S., and Khurelbaatar,
B. (2021) Geochemistry and geochronology of granitoid rocks of the Taatsiin Gol pluton of the Khangai
Complex, Central Mongolia.
Mongolian Geoscientist, 26 (53), 18-36.
Fig. 2 is the geologic map in
the area.
https://www.mongoliajol.info/index.php/MGS/article/view/1788/1969
Taatsiin
Gol pluton of the Khangai Complex (230-256)
The owner of this website (Takahashi) represents a
description with the way of Glanzner et al.
(2019) and Ishihara (1977).
Petrography:
1-st Diorite;
(bt-hbl 5-7, 5, 63-66, 30-35 diorite)
2-nd granodiorite; (ttn bearing bt-hbl 15-20,
10-15, 30-35, 20-30 granodiorite)
3-rd; (ttn
bearing bt 30, 38-45, 20-25, 5-7 granite)
Granitoids series: Ilmenite series from ilmenite in 2-nd
phase and no opaque in 3-rd.
(9) Pavel Hanžl,
Karel Schulmann, Vojtěch Janoušek, Ondrej Lexa, Kristýna Hrdličková, Yingde Jiang, David Buriánek1, Battushig
Altanbaatar, Turbat Ganchuluun, Vojtěch Erban (2016) Making continental crust: origin of Devonian
orthogneisses from SE Mongolian Altai.
Journal of Geosciences, 61, 25-50.
www.jgeosci.org/content/jgeosci.206_hanzl.pdf
(10)
David
Buriánek, Vojtěch Janoušek, Pavel Hanžl, Yingde Jiang, Karel Schulmann, Ondrej Lexa, Battushig Altanbaatar (2016) Petrogenesis of the Late Carboniferous Sagsai Pluton in the SE Mongolian Alta. Journal of Geosciences, 61, 67-92.
www.jgeosci.org/content/jgeosci.207_burianek.pdf