DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION
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3 Institute of Geology Karelian Research Centre of RAS DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION Papers of all-russian Conference with participation of foreign scientists Petrozavodsk 2017
4 2017
5 Deep structure and geodynamics of the Lake Ladoga area Proceedings of the International C This volume consists of the P
6 ( )
7 2 2 METASOMATISM AND FLUID MODE OF RAAHE-LADOGA ZONE AS CONTACT TERRAIN OF CRATON AND MOBILE BELT Abstract
8 7
9 II
10 FRACTAL CHARACTERISTICS OF THE ONEGO-LADOGA HYDROGRAPHIC NETWORK AND SEDIMENTATION Abstract
11 10
12 11
13 12 N N ln lnn
14 Таблица o
15 Series of the ratio the thickness of the and the thickness of the annual layer of the
16 f
17
18 17 Tur
19 1 1 2 CONSTRUCTION OF THREE-DIMENSIONAL GEOELECTRIC MODEL OF THE LAKE LADOGA CONDUCTIVITY ANOMALY AREA 1, 1 2 Abstract th
20 19
21 20
22 21
23 22 model in the section along the
24
25
26 C
27 T A A Kovtun A A Palshin N A Smirnov Tokarev A Asming L L I L the
28 ON THE CREATION OF A DIGITAL MODEL OF CORE OF TERRIGENOUSRESERVOIRSFOR SOLVING EXPLORATION PROBLEMS Abstract
29 Coremodel
30 29
31 Таблица L 229
32
33 the cumulative volume ó ó r r
34
35 7 9
36
37 1, ELECTRICAL PROFILING BY THE METHOD OF EXTERNAL SLIDING DIPOLE (MESD) ON THE ROAD OF HIITOLA-SUISTAMO 1, Abstract
38 9 2 Position of the The circles indicate the
39 MN MN GPS
40 M1N1 M1N2 N1N2 M 1N 1 M 1 I 2 2 N 2 1 M 1N 1 M 1N 1 l 1 1 M N M 1N 2 M 1N 2 l 1 2 M N A B ~ r ~ r r r 0 r r r
41 r A r B r A > r B r A r B
42 MN
43
44 1,2 SOME FEATURES OF ELECTRICAL CONDUCTIVITY OF UKRAINIAN AND BALTIC SHIELDS 1 2
45 Ukrainian crystal shield
46
47 S 1
48
49 L L2 Baltic Array Research CS normal
50
51 F
52
53
54
55
56 1,2 ELECTRICAL CONDUCTIVITY OF UKRAINIAN AND BALTIC SHIELDS 1,2 1 2 of S 1 values of S 1 1 in the local sections of 1 S 1
57
58 I II III S 1 S 2 Korosten Korsun Novomirgorodsky Priazovsky fault zones a inter and intra suture zones in Golovanevskaya Inguletsko Krivoy Rog Pavlogradskaya I II Podolsky III Rosinsky Bug Ingul Priazovsky volcano Roman numerals in circles indicate some geotransects 1 2 S 1 S 1 S 1
59 S 1
60
61 S S 1
62 L L Baltic Array Research CS normal
63 Fennoscandian conductivity from Natural and Induction Control Soundings
64 F
65
66
67 T
68 ELECTROMAGNETIC STUDIES ON THE TERRITORY OF THE VCM Abstract
69 Lemi
70 . 1. An entry of the electromagnetic xy yx
71 im root of the
72 71
73 INVESTIGATION OF THE MULTI-DIMENSIONAL FRACTURING OF Abstract
74
75
76
77
78 77 P P 1 1 R 2 P P Circle diagram of the fracturing reconstructed fracturing P P 1 and tectonic dislocation R 1 and R 2 measurments of the fracture orientation area fracturing P P 1 fractur ing R 1 R 1 tectonic dislocation trend R 2 R 2 disloca tion trend
79 Position of the
80 79 selection on the and circle diagrams of microfracturing
81 orientation diagrams left and right methods
82
83
84 MAJOR METALLOGENIC SYSTEMS IN THE LAKE LADOGA AREA
85
86 Таблица
87 Pd Au Sn Zn In Be u Fe Ag Au Pt Ta Li Ti P -
88 PR
89 Fe Cu Sn Ag - Pd Pt
90 C C
91 90
92 ITEGRATED SEISMOLOGICAL AND SEISMIC STUDIES OF THE DEEP STRUCTURE OF THE SOUTH SLOPE OF THE BALTIC SHIELD most important problems in modern solid earth sciences big deposits
93 92 I II
94 Ladoga area
95 I II. 2.
96 S
97
98 97
99
100 APPLICATION OF DC RESISTIVITY MULTI-ELECTRODE ELECTRICAL EXPLORATION FOR THE STUDY OF A LOCAL ELEMENT ON THE NORTHEASTERN EDGE OF THE LADOGA ELECTRICAL CONDUCTIVITY ANOMALY Abstract
101 100
102 101 N i M M
103 102
104 Golden Surfer
105
106
107 ORE SPECIFICITY OF THE GRANITE-GNEISS DOME STRUCTURE RIMS OF NORTH LADOGA REGION Abstract 1 1 AR PR 1 PR 1
108 107 Fe Cu Co Ni Cr S Cr Fe Co
109 U Ni S Ca U Sr Cu S
110 109
111 ..ru RARE-EARTH MINERALIZATION OF ALKALINE AND MODERATELY ALKALINE INTRUSIVE COMPLXES mineral associations in alkaline and moderately alkaline massifs in the northern Lake 2
112 111 K 2 Na 2 K 2 P 2 Sr Ba Na TR Ba Sr P Ti Sr Ba Ba Sr P Ti Таблица 1 P 2 2 La Ce
113 112 Ta Ga Th Sr Ba R R Sr
114 Th Ba Sr Ca Sr Ba Ti P Ta Sr Ba Be Sn Bi Th U
115 h U
116 1, , 1 1, THE RESULTS OF EM STUDY OF BARYATINSKAYA CRUSTAL HIGH-CONDUCTIVE ANOMALY 1, , Abstract 2
117
118 117
119
120 119
121 120 a
122 121
123 122
124 d d
125
126 NOBLE-METAL MINERALIZATION OF THE KAALAMO COMPLEX AND THE VÄLIMÄKI MASSIF Abstract
127
128 127 AR 2 Rh Ir Cr Ni Co Ni
129 Ni Ni Co Cu Ni Ni Co Ni Cu K Co Cu Ni Co Ag Te Bi As Se Sn Au Pt Pd Ru Rh Pt Pd Pt Pd
130 Fe Ti Cu S Au Pt Pd Rh Cu Cu S
131
132 1 2 ACCRETIONARY OROGEN AND ADJACENT MARGIN MT SOUNDING AND DENSITY MODELING _ 1 2
133
134 C
135
136 a a
137
138 See
139 Acknowledgments
140
141 STUDYING OF PETROPHYSICAL PROPERTIES OF SALMINSKI MASSIFF GRANITES BY LABORATORY METHODS Abstract
142 I
143 s
144 Таблица Таблица
145
146
147 YOUNG TECTONIC AND SEISMICITY
148
149
150
151
152
153
154 II
155 «LEMI GI-MTS-1» THE MAGNETOTELLURICAL OBSERVATIONS BY LEMI AND GI-MTS-1 STATIONS RESULTS COMPARISON IN THE NORTHERN LADOGA REGION GI
156 Таблица 1
157 GI
158 OF THE LAKE LADOGA AREA ON THE COMPLEX OF GEOLOGICAL-GEOPHYSICAL DATA
159
160 the territory of Ladoga
161
162 Luosto Tiira et al
163
164 SOUNDINGS OF INHOMOGENEOUS MEDIA APPLICABLE TO THE SOLUTION OF GEOLOGICAL PROBLEMS Abstract
165
166 of a homogeneous medium
167 2 1 I II
168
169
170
171 170
172 171
173 LADOGA VOLCANO-TECTONIC STRUCTURE (GEOLOGICAL STRUCTURE) The geological structure and individual characteristics of the Ladoga structure
174
175
176
177
178 177
179 ± ± Sm Nd ± ± 0
180 179
181 MINERALOGENY OF THE LADOGA VOLCANO-TECTONIC STRUCTURE Abstract
182
183 Sr Ba P 2
184
185 Cu Ni Co 2
186 Ni Co
187 2
188
189 1 1 PRIMAL RESULTS OF AUDIOMAGNETOTELLURICS SOUNDING ON SITES OF LOW RESISTIVITY 1 1 Abstract
190
191 190
192 191
193 192
194
195
196 GEOPHYSICAL METHOD FOR INTERPRETATION OF THE TECTONIC VYBORG RAPAKIVI GRANITE MASSIF Abstract
197
198 197 1 R 1
199 2 R 1 R 1
200 199
201 200 Scheme of the anomaly
202 201 resistance sections for
203 202
204 22
205 1 2 THE SOUTH-EASTERN BALTIC SHIELD CRUSTAL STRUCTURE, 1 2 Abstract
206
207
208 207
209
210 209
211 210
212 211
213 212
214 -
215
216 CHARACTERISTICS OF SEISMIC NOISE ON SITES OF LADOGA LAKE REGION AND ESTIMATION OF THE ITS ENDOGENIC COMPONENT Abstract
217 The scheme of sites of
218
219 mic noise on sites of southeast Fennoscandian Shield in night ginnings of registration of seismic
220 219
221 220
222 221 noise on a site of Caves Inostranceva
223 222
224
225 DATA ACROSS LAKE LADOGA CONDUCTIVITY ANOMALY Abstract
226
227
228 227
229
230 229
231
232 VELOCITIES FLOORS OF THE MANTLE UNDER FENNOSCANDIA ACCORDING TO SEISMOTOMOGRAPHY
233 z z z
234 II
235
236 . 2. The roof and the regions constant gradient on the of the mantle and transition zone the mantle
237
238 I I II
239 INTEGRO GIS INTEGRO AS A TOOL FOR COMPILATION OF COMPLEX GEOLOGICAL MODEL Abstract
240
241
242
243 . 1. of source data in 2 Scenes of GIS
244
245 BASIC MAGMATIC COMPLEXES OF THE VORONEZH CRYSTALLINE MASSIF AND ITS REFLECTION IN GEOPHYSICAL FIELDS
246
247 Ar 1-10 g a a g a 10
248 g a a g g
249 g g a g a g a a g a a g a a a a g a a
250
251
252 DEEP SEISMIC STUDIES IN THE SOUTHEASTERN FENNOSCANDIAN SHIELD
253
254
255
256 2
257 I I I
258 2 2
259 Structural scheme of Fennoscandian Shield
260
261 THE MEASUREMENTS OF CSAMT AND AMT-MT ELECTROMAGNETIC FIELDS ON THE NORTH-EASTERN EDGE OF THE LADOGA ANOMALY Abstract grounded sections of industrial transmission lines located on the Kola Peninsula in the a
262 L Phoenix 2 0 T T 0 arg
263
264 L Phoenix L
265
266 L The resistivity curves and curves for registered of the for at a Ladoga
267 K
268 ELECTRICAL CONDUCTIVITY AS THE MANIFESTATION OF THE GEODYNAMIC PROCESSES IN THE GOLOVANIVSK SUTURE ZONE 1 A Abstract rocks and metasomatic agneto methods in o the of the sedimentary rocks of the o and the o margin anomalies in Golovanivsk
269
270
271 270
272
273 272
274
275
276
277 MINERAGENIC AND RESOURCE POTENTIAL OF INDUSTRIAL MINERALS IN THE SWEKOFENNIAN PROVINCE (ADOPERATION) Abstract
278 277 2
279 Таблица Al 2 Fe 2 Na 2 K
280 279 0
281 2
282
283
284 Таблица 2 >
285 2 2 2
286 Fe 2
287
288 STUDY OF THE DEEP CONDUCTIVITY STRUCTURE OF THE Summary Introduction 7 2
289 Applied technique Application in the ladoga project N and 21 Conclusions
290 1
291 290 Conductance model and the data and model Re modelling of the geoelectric crustal structure of Ladoga Lake anomaly according 10 induction vectors at the
292 291 References P
293 ELECTROMAGNETIC STUDY OF LITHOSPHERIC STRUCTURE OF MARGINAL ZONE OF THE EAST EUROPEAN CRATON IN NW POLAND Summary Introduction
294 The methods
295
296 Results
297 the largest singular values of the
298 297 Acknowledgments References
299 DEEP LITHOSPHERIC STRUCTURE BENEATH THE POLISH PART OF THE EAST EUROPEAN CRATON AS A RESULT OF INTEGRATED 1-D AND 2-D MT DATA INTERPRETATION Summary Introduction Archean and early Proterozoic crystalline crust consists mainly of granites and
300 299 The methods
301 m has Results
302 1
303
304 Acknowledgments
305 References
306 THREE-DIMENSIONAL ELECTRICAL RESISTIVITY MODEL OF THE POMERANIA REGION IN NW POLAND ul. Summary goal task Introduction
307 study and include recently collected data The methods Results The resulting model of electrical resistivity ig
308
309 . Acknowledgments References
310 Res The conductivitystruc.
311
312 110 GI 172
313
314 292
315 CONTENT 9 27 Ivanov
316 110 Lavrov and 172
317 BASIC Shyrkov B I Burakhovych T K Kushnir A N
318 292
319 DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION C 1
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