DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION

Size: px

Start display at page:

Download "DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION"

Shanon Parsons
6 years ago
Views:

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

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

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

33 the cumulative volume ó ó r r

35 7 9

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

44 1,2 SOME FEATURES OF ELECTRICAL CONDUCTIVITY OF UKRAINIAN AND BALTIC SHIELDS 1 2

45 Ukrainian crystal shield

47 S 1

49 L L2 Baltic Array Research CS normal

51 F

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

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

61 S S 1

62 L L Baltic Array Research CS normal

63 Fennoscandian conductivity from Natural and Induction Control Soundings

64 F

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

$77 P P 1 1 R 2 P P 1 1 1 2 2 Circle diagram of the fracturing reconstructed fracturing P P 1 and tectonic dislocation R 1 and R 2$

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

84 MAJOR METALLOGENIC SYSTEMS IN THE LAKE LADOGA AREA

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

98 97

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

LATE ARCHAEAN FELSIC ALKALINE MAGMATISM: GEOLOGY, GEOCHEMISTRY, AND TECTONIC SETTING

LATE ARCHAEAN FELSIC ALKALINE MAGMATISM: GEOLOGY, GEOCHEMISTRY, AND TECTONIC SETTING ZOZULYA DMITRY 1, EBY NELSON 2 1 - Geological Institute Kola Science Centre RAS, Apatity, Russia 2 - Department of Environmental,