Environmental Engineering Reference
In-Depth Information
Table 5.2 ( cont. )
DG and ID statistics
Flow a
N DG ( N ID ) D ( )
I ( )
95 ( )
nn
DG (ID)
K
α
16
nd9
nd8
DG9
2
31.3
68.0
624.9
4.0
-
17
nd7
nd6
DG10
2
9.4
70.6
1012.6
3.1
-
18
nd5
nd4
DG11
2
62.2
73.7
433.6
4.8
-
19
nd3
ID8
7
40.0
81.0
634.9
2.1
20
nd1
ID9
8
100.0
73.0
1088.9
1.5
21
mr1
mr4
DG12
4
89.0
78.1
692.5
2.7
-
Abagalakh section (70.4 N, 90.1 E)
22
mr5
mr6
DG13
2
159.9
82.3
789.6
3.5
-
23
mr7
mr9
DG14
3
86.4
75.9
261.3
5.0
-
24
mr10
mr12
DG15
4
120.0
77.3
340.2
3.8
-
25
mk3
ID10
9
161.0
75.0
277.8
2.8
26
mk4
mk5
DG16
2
75.5
73.2
657.7
3.9
-
27
mk6
mk8
DG17
3
105.8
79.5
225.7
5.4
-
28
mk9
ID11
9
68.0
67.0
188.4
3.4
29
mk10
mk13
DG18
4
93.5
70.8
191.9
5.1
-
30
hr1
hr2
DG19
2
89.0
57.1
440.4
4.7
-
31
hr3
-
hr4
DG20
2
107.1
65.0
260.4
6.1
32
hr5
ID12
8
96.0
73.0
56.2
6.6
33
hr7
-
hr8
DG21
2
53.4
78.0
264.8
6.1
34
km1
-
km5
DG22
4
71.7
72.3
2423.2
1.4
35
km6
-
km7
DG23
2
42.5
75.6
173.9
7.5
Talnakh section (69.5 N, 88.7 E)
1
ta8
ID
8
146.0
58.0
84.0
5.4
2
ta7
ID
8
152.0
49.0
56.2
6.6
3
ta6
ID
6
166.0
56.0
17.2
13.8
4
ta5
ID
4
195.0
61.0
3402.8
1.2
5
ta4
ID
8
280.0
78.0
43.6
7.5
6
ta3
ID
7
236.0
66.0
72.8
6.2
Mean b
18
88.1
75.6
68
4.2
a See Table 5.1 for further details and abbreviations.
b DG and ID mean paleomagnetic direction for the composite Norilsk section, calculated
without reversal, transitional and excursional directions (for details see text and the
discussion in Pavlov et al ., 2011 : paleomagnetic directions from DG11
DG23
stratigraphic interval only have been used. Corresponding paleomagnetic pole is:
S lat ¼
-
70.0 , S long ¼
89.3 , P l at ¼
57.2 , P long ¼
146.9 , dp/dm
7.1 /7.8 .
¼
The reversed interval of the Sunduk section includes the two lowermost
reversely magnetized
ows
(ID1, DG2, DG3, DG4, DG5) make up the transitional interval. Excursional
directions (identified as it was done by Heunemann et al .( 2004 ) and Gurevitch
et al .( 2004 )) are recorded by flows in DG8 and ID6. Similarly to the section
studied by Heunemann et al .( 2004 ), in the Sunduk section between the transitional
flows that form the volcanic pulse DG1. The next 17
Search WWH ::




Custom Search