влияние четвертичного похолодания в северных районах

5.
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1987ν
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, 1998).
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Дβ, γЖ
1β1,
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1.
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121
1β1
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Д5Ж
Д6Ж.
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ν 90 0
β470 – 103 0 (
β6β0 – 106 0 (
9
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2430
15.0
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–
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Д6Ж.
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362
β4
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88,γ ° .
99,β °
54,8
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β6β0
β470 ,
2
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94.5
94.2
93.8
93.3
86.1
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80.8
79.6
77.0
74.2
71.5
69.1
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97.2
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91.9
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52.5
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90.6
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92.9
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100.3
97.5
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90.7
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/ β
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89.5
89.4
89.4
89.4
89.4
89.4
89.4
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88.3
87.9
87.5
80.2
76.1
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(10γ° )
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100.γ °
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(β6β0
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μ 1)
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5.
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363
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1.
134 .
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2.
– 222 .
.–
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5.
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. .
. .
. .
3.
4.
//
. .
.
, 2004. – . 23. –
.,
. .,
5. – . 111–115.
. .,
.:
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6.
(
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) //
.
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.
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,
,
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-
 I (P )  f
,
N 
k 1
t−t0,
m
μ
Д1, 2].
,
N
– N 6. –
6. – .1070-1078.
)
g[t−t0Ж.
g[t−t0Ж
t t0.
.
, 1986.
, 2002.
.
(
.:
. .
. .
, 1997. – . 38. -
.
, 1987. –
, 1974. – 123 .
//
. 48-54.
:
,
S,
,
 X k ,Yk , Z k , t  I k ,
(1)
ν  X k ,Yk , Z k , t  –
f–
I k –
ν
,
.
Vzzk[t−t0Ж
(1)
.
(1),
,
,
[1, 2Ж
Vxxk[t−t0Ж,
,
Vyyk[t−t0],
,
.
,
,
[3, 4Ж,
.
,
.
.
Дγ, 4,Ж
.
Vx,
.
Vy,
Vz,
(
Vxx[t−t0Ж,
Vyy[t−t0Ж,
50 %, 75 % 100 %
(
Vzz[t−t0]),
)
. 1
10 .
.