richard
richard
2015-05-21T18:27:23Z
15.00
12435
28800
0
0
False
False
Mongolia |
Latitude |
Longitude |
Temp. |
Heat |
Data |
descriptive |
Site |
(degrees) |
(degrees) |
Elevation |
Minimum |
Maximum |
Number of |
Gradient |
Number |
Conductivity |
Number of |
Production |
Heat Flow |
Number |
Reference |
Year of |
Number |
code |
Name |
(+N, -S) |
(+E, -W) |
(meters) |
Depth (m) |
Depth (m) |
Temps. |
(mK/m) |
of Conductivities |
W/m/K |
Heat Prod. |
10 -6W/m |
mW/m2 |
of Sites |
Number |
Publication |
Comments |
MN 1 |
EBKNAB |
HUBSUGO1 |
50.95 |
100.4 |
1785 |
-230 |
1 |
75 |
1.2 |
83 |
1 |
91 |
86 |
MN 2 |
EBKNAB |
HUBSUGO2 |
50.982999999999997 |
100.38 |
1785 |
-220 |
1 |
50 |
1.1000000000000001 |
60 |
1 |
91 |
86 |
MN 3 |
EBKNAB |
HUBSUGO3 |
51 |
100.33 |
1785 |
-180 |
0 |
74 |
1 |
74 |
1 |
91 |
86 |
MN 4 |
EBKNAB |
HUBSUGO4 |
51 |
100.38 |
1785 |
-215 |
1 |
83 |
1 |
83 |
1 |
91 |
86 |
MN 5 |
EBKNAB |
HUBSUGO5 |
51.167000000000002 |
100.45 |
1785 |
-215 |
1 |
120 |
1 |
120 |
1 |
91 |
86 |
MN 6 |
EBKNAB |
HUBSUGO6 |
51.116999999999997 |
100.45 |
1785 |
-209 |
1 |
113 |
1 |
113 |
1 |
91 |
86 |
MN 7 |
EBKNAB |
HUBSUGO7 |
51 |
100.47 |
1785 |
-218 |
1 |
130 |
1 |
130 |
1 |
91 |
86 |
MN 8 |
EBKNAB |
HUBSUGO8 |
51 |
100.52 |
1785 |
-205 |
1 |
500 |
1 |
500 |
1 |
91 |
86 |
MN 9 |
EBKNAB |
HUBSUGO9 |
51.017000000000003 |
100.55 |
1785 |
-155 |
1 |
0 |
1 |
1 |
91 |
86 |
MN 10 |
EBKNAB |
ARDAG-PH |
50.683 |
100.22 |
20 |
180 |
21 |
2.9 |
61 |
1 |
90 |
86 |
MN 11 |
EBKNAB |
ERDENTUI |
49 |
104.17 |
1300 |
10 |
150 |
14 |
2.84 |
40 |
1 |
90 |
86 |
MN 12 |
EBKNAB |
IH-HAIRH |
46.917000000000002 |
106 |
1400 |
10 |
170 |
22 |
2.93 |
65 |
4 |
90 |
86 |
MN 13 |
EEABIA |
SHAND22 |
48.768000000000001 |
104.2 |
1110 |
20 |
340 |
30 |
16 |
21 |
2.6 |
3 |
1 |
42 |
2 |
90 |
86 |
MN 14 |
EEABIB |
BORU717 |
46.252000000000002 |
109.25 |
1313 |
20 |
130 |
42 |
25 |
34 |
3.23 |
7 |
0.8 |
71 |
5 |
90 |
86 |
MN 15 |
EEABIB |
DELG176 |
47.734999999999999 |
111.28 |
1168 |
20 |
140 |
20 |
13 |
25 |
2.38 |
4 |
1.3 |
31 |
2 |
90 |
86 |
MN 16 |
EFABEB |
BERC200 |
47.801000000000002 |
111.18 |
1157 |
20 |
130 |
12 |
25 |
16 |
2.0299999999999998 |
3 |
1.3 |
46 |
1 |
90 |
86 |
MN 17 |
EFABIB |
TSAG116 |
46.334000000000003 |
110.17 |
1295 |
40 |
140 |
11 |
34 |
5 |
1.84 |
66 |
1 |
90 |
86 |
MN 18 |
EBABEB |
KHUBS5 |
50.683999999999997 |
100.22 |
1830 |
20 |
180 |
17 |
20 |
3 |
60 |
1 |
90 |
86 |
MN 19 |
EBABEB |
BURENC1 |
49.767000000000003 |
99.933000000000007 |
1670 |
20 |
220 |
61 |
20 |
38 |
2.9 |
5 |
1.1000000000000001 |
78 |
4 |
90 |
86 |
MN 20 |
EEABIB |
TAWA489 |
43.6 |
105.43 |
1520 |
20 |
130 |
46 |
10 |
38 |
1.62 |
10 |
0.7 |
16 |
6 |
90 |
86 |
MN 21 |
EEABFB |
SUBU140 |
43.85 |
108.38 |
985 |
20 |
180 |
22 |
22 |
15 |
1.79 |
2 |
1.1000000000000001 |
41 |
2 |
90 |
86 |
MN 22 |
EEABIB |
OJUT102 |
44.883000000000003 |
109.47 |
1100 |
20 |
70 |
5 |
14 |
10 |
2.02 |
28 |
1 |
90 |
86 |
MN 23 |
EEABEB |
DUNDB21 |
48.219000000000001 |
111.19 |
1148 |
20 |
100 |
15 |
30 |
12 |
3.13 |
100 |
2 |
90 |
86 |
MN 24 |
EEABIB |
NARIN10 |
48.317 |
109.65 |
1495 |
20 |
90 |
14 |
24 |
4 |
2.54 |
61 |
2 |
90 |
86 |
MN 25 |
EEABGB |
UNDUR28 |
47.868000000000002 |
110.17 |
1480 |
20 |
360 |
70 |
25 |
16 |
2.85 |
5 |
1 |
74 |
2 |
90 |
86 |
MN 26 |
EEABGB |
DZANS20 |
47.234000000000002 |
111.59 |
1215 |
30 |
190 |
41 |
18 |
25 |
2.59 |
45 |
3 |
90 |
86 |
MN 27 |
EEABFB |
ICHSHA4 |
43.634999999999998 |
105.97 |
1680 |
20 |
100 |
17 |
12 |
20 |
2.76 |
33 |
2 |
90 |
86 |
MN 28 |
EEABFB |
SHUTE20 |
43.982999999999997 |
107.72 |
1135 |
20 |
80 |
18 |
14 |
2.76 |
44 |
3 |
90 |
86 |
MN 29 |
EZAEBA |
TSAGAN-S |
43.917000000000002 |
108.25 |
1000 |
25 |
2 |
2.16 |
54 |
1 |
92 |
75 |
MN 30 |
EZAEBA |
ARDAG-5 |
51.133000000000003 |
100.27 |
1950 |
21 |
4 |
2.5499999999999998 |
54 |
1 |
92 |
75 |
MN 31 |
EZAEBA |
ERDENTUI |
49 |
104.17 |
1600 |
12 |
2 |
2.85 |
34 |
1 |
92 |
75 |
MN 32 |
EZAEBA |
HARCHULU |
46.917000000000002 |
106 |
1400 |
22 |
5 |
2.93 |
65 |
1 |
92 |
75 |
MN 33 |
EZAEBA |
IH-HAIRH |
46.917000000000002 |
106 |
1400 |
32 |
4 |
2.62 |
84 |
1 |
92 |
75 |
MON001 |
E B |
BURINKHA |
49.767000000000003 |
99.933000000000007 |
1670 |
20 |
220 |
4 |
20 |
2.9 |
78 |
1 |
1 |
88 |
58 |
MON002 |
E B |
ARDAG-KH |
50.683 |
100.22 |
1830 |
20 |
180 |
1 |
21 |
2.9 |
61 |
1 |
1 |
88 |
61 |
MON003 |
E B |
SHAND-CM |
48.767000000000003 |
104.22 |
1110 |
20 |
340 |
2 |
16 |
2.6 |
42 |
1 |
1 |
88 |
42 |
MON004 |
E |
ERDENETU |
49 |
104.17 |
1300 |
10 |
150 |
1 |
14 |
2.84 |
40 |
1 |
1 |
88 |
MON005 |
E |
IKH-KHAI |
46.917000000000002 |
106 |
1400 |
10 |
170 |
4 |
22 |
2.93 |
65 |
1 |
1 |
88 |
MON006 |
E B |
NARINGYI |
48.317 |
109.67 |
1495 |
20 |
90 |
2 |
24 |
2.54 |
61 |
1 |
1 |
88 |
61 |
MON007 |
E B |
UNDUR-TS |
47.866999999999997 |
110.17 |
1480 |
20 |
360 |
3 |
25 |
2.85 |
74 |
1 |
1 |
88 |
84 |
MON008 |
E B |
DUND-BUL |
48.232999999999997 |
111.2 |
1148 |
20 |
100 |
2 |
30 |
3.13 |
100 |
1 |
1 |
88 |
94 |
MON009 |
E B |
DELGERKH |
47.75 |
111.28 |
1168 |
20 |
140 |
2 |
13 |
2.38 |
31 |
1 |
1 |
88 |
31 |
MON010 |
E B |
BERKH-CM |
47.8 |
111.18 |
1157 |
20 |
130 |
1 |
25 |
2.0299999999999998 |
46 |
1 |
1 |
88 |
51 |
MON011 |
E B |
DZAN-SHI |
47.232999999999997 |
111.6 |
1265 |
30 |
190 |
3 |
18 |
2.59 |
45 |
1 |
1 |
88 |
47 |
MON012 |
E B |
BORONNDU |
46.267000000000003 |
109.25 |
1313 |
20 |
130 |
5 |
25 |
3.23 |
71 |
1 |
1 |
88 |
81 |
MON013 |
E B |
TSAGAN-E |
46.332999999999998 |
110.17 |
1295 |
40 |
140 |
1 |
34 |
1.84 |
65 |
1 |
1 |
88 |
62 |
MON014 |
E B |
TAVAN-TO |
43.6 |
105.43 |
1520 |
20 |
130 |
6 |
10 |
1.62 |
16 |
1 |
1 |
88 |
16 |
MON015 |
E B |
IKH-SHAN |
43.633000000000003 |
105.98 |
1680 |
20 |
100 |
2 |
12 |
2.76 |
33 |
1 |
1 |
88 |
31 |
MON016 |
E B |
TSAGAN-S |
43.85 |
108.38 |
985 |
20 |
180 |
3 |
22 |
1.79 |
41 |
1 |
1 |
88 |
38 |
MON017 |
E B |
SHUTEN-S |
43.982999999999997 |
107.72 |
1135 |
20 |
80 |
3 |
14 |
2.76 |
44 |
1 |
1 |
88 |
38 |
MON018 |
E B |
OYUT-SM- |
44.883000000000003 |
109.47 |
1100 |
20 |
80 |
1 |
14 |
2.02 |
28 |
1 |
1 |
88 |
28 |
188 KHUTORSKOY, M.D., AND V.V. YARMOLUK |
HEAT FLOW, STRUCTURE AND EVOLUTION OF THE LITHOSPHERE OF MONGOLIA. |
SUBMITTED TO TECTONOPHYSICS, 1988. |
{COMMENT: MEASURED HEAT FLOW} |
False
False