DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION

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

2017

Deep structure and geodynamics of the Lake Ladoga area Proceedings of the International C This volume consists of the P

(1928 2016)

2 1.b.yu@mail.ru 2 METASOMATISM AND FLUID MODE OF RAAHE-LADOGA ZONE AS CONTACT TERRAIN OF CRATON AND MOBILE BELT 1 2 1 2 Abstract

7

II

FRACTAL CHARACTERISTICS OF THE ONEGO-LADOGA HYDROGRAPHIC NETWORK AND SEDIMENTATION Abstract

10

11

12 N N ln lnn

Таблица 1 1 2 o

Series of the ratio the thickness of the and the thickness of the annual layer of the

f

17 Tur

1 1 2 CONSTRUCTION OF THREE-DIMENSIONAL GEOELECTRIC MODEL OF THE LAKE LADOGA CONDUCTIVITY ANOMALY AREA 1, 1 2 Abstract th

19

20

21

22 model in the section along the

C

T A A Kovtun A A Palshin N A Smirnov Tokarev A Asming L L I L the

ON THE CREATION OF A DIGITAL MODEL OF CORE OF TERRIGENOUSRESERVOIRSFOR SOLVING EXPLORATION PROBLEMS Abstract

Coremodel

29

Таблица 1 10 2 L 229

the cumulative volume ó ó r r

7 9

1,2 2 1 2 ELECTRICAL PROFILING BY THE METHOD OF EXTERNAL SLIDING DIPOLE (MESD) ON THE ROAD OF HIITOLA-SUISTAMO 1,2 2 1 2 Abstract

9 2 Position of the The circles indicate the

MN MN GPS

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

r A r B r A > r B r A r B

MN

1,2 1. @mail.ru 2 @. SOME FEATURES OF ELECTRICAL CONDUCTIVITY OF UKRAINIAN AND BALTIC SHIELDS 1 2

Ukrainian crystal shield

S 1

L L2 Baltic Array Research CS normal

F

1,2 1. @mail.ru 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

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

S 1

S S 1

L L Baltic Array Research CS normal

Fennoscandian conductivity from Natural and Induction Control Soundings

F

T

1 2 1 2 ELECTROMAGNETIC STUDIES ON THE TERRITORY OF THE VCM 1 2 1 2 Abstract

Lemi

. 1. An entry of the electromagnetic xy yx

70. 2. im root of the

71

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 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

Position of the

79 selection on the and circle diagrams of microfracturing

orientation diagrams left and right methods

MAJOR METALLOGENIC SYSTEMS IN THE LAKE LADOGA AREA

Таблица

Pd Au Sn Zn In Be u Fe Ag Au Pt Ta Li Ti P -

PR

Fe Cu Sn Ag - Pd Pt

C C

90

1 2 1 1 2 ITEGRATED SEISMOLOGICAL AND SEISMIC STUDIES OF THE DEEP STRUCTURE OF THE SOUTH SLOPE OF THE BALTIC SHIELD 1 2 1 1 2 most important problems in modern solid earth sciences big deposits

92 I II

Ladoga area

I II. 2.

S

97

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

100

101 N i M M

102

Golden Surfer

ORE SPECIFICITY OF THE GRANITE-GNEISS DOME STRUCTURE RIMS OF NORTH LADOGA REGION Abstract 1 1 AR PR 1 PR 1

107 Fe Cu Co Ni Cr S Cr Fe Co

U Ni S Ca U Sr Cu S

109

..ru RARE-EARTH MINERALIZATION OF ALKALINE AND MODERATELY ALKALINE INTRUSIVE COMPLXES mineral associations in alkaline and moderately alkaline massifs in the northern Lake 2

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

112 Ta Ga Th Sr Ba R R Sr

Th Ba Sr Ca Sr Ba Ti P Ta Sr Ba Be Sn Bi Th U

h U

1,2 2 1 1, 1 1,2 1 1 2 THE RESULTS OF EM STUDY OF BARYATINSKAYA CRUSTAL HIGH-CONDUCTIVE ANOMALY 1,2 2 1 1 1 1,2 1 1 2 Abstract 2

117

119

120 a

121

122

d d

1 1 2 1 2 NOBLE-METAL MINERALIZATION OF THE KAALAMO COMPLEX AND THE VÄLIMÄKI MASSIF 1 1 2 1 2 Abstract

127 AR 2 Rh Ir Cr Ni Co Ni

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

129 2 2 Fe Ti Cu S Au Pt Pd Rh Cu Cu S

1 mints@.ru 2 ACCRETIONARY OROGEN AND ADJACENT MARGIN MT SOUNDING AND DENSITY MODELING _ 1 2

C

a a

See

Acknowledgments

STUDYING OF PETROPHYSICAL PROPERTIES OF SALMINSKI MASSIFF GRANITES BY LABORATORY METHODS Abstract

I

s

Таблица 1 122 10 Таблица 2 2917

YOUNG TECTONIC AND SEISMICITY

II

«LEMI GI-MTS-1» THE MAGNETOTELLURICAL OBSERVATIONS BY LEMI AND GI-MTS-1 STATIONS RESULTS COMPARISON IN THE NORTHERN LADOGA REGION GI

Таблица 1

GI

1 1 1 2 OF THE LAKE LADOGA AREA ON THE COMPLEX OF GEOLOGICAL-GEOPHYSICAL DATA 1 1 2 1 2

the territory of Ladoga

Luosto Tiira et al

SOUNDINGS OF INHOMOGENEOUS MEDIA APPLICABLE TO THE SOLUTION OF GEOLOGICAL PROBLEMS Abstract

of a homogeneous medium

2 1 I II

170

171

LADOGA VOLCANO-TECTONIC STRUCTURE (GEOLOGICAL STRUCTURE) The geological structure and individual characteristics of the Ladoga structure

177

± ± Sm Nd ± ± 0

179

MINERALOGENY OF THE LADOGA VOLCANO-TECTONIC STRUCTURE Abstract

Sr Ba P 2

Cu Ni Co 2

Ni Co

2

1 1 PRIMAL RESULTS OF AUDIOMAGNETOTELLURICS SOUNDING ON SITES OF LOW RESISTIVITY 1 1 Abstract

190

191

192

1 1 1 2 1 2 GEOPHYSICAL METHOD FOR INTERPRETATION OF THE TECTONIC VYBORG RAPAKIVI GRANITE MASSIF 1 1 1 2 1 2 Abstract

197 1 R 1

2 R 1 R 1

199

200 Scheme of the anomaly

201 resistance sections for 2 2 2 2

202

22

1 2 THE SOUTH-EASTERN BALTIC SHIELD CRUSTAL STRUCTURE, 1 2 Abstract

207

209

210

211

212

-

1 2 1 2 CHARACTERISTICS OF SEISMIC NOISE ON SITES OF LADOGA LAKE REGION AND ESTIMATION OF THE ITS ENDOGENIC COMPONENT 1 2 1 2 Abstract

The scheme of sites of

217 10 2 2 2

mic noise on sites of southeast Fennoscandian Shield in night ginnings of registration of seismic

219

220

221 noise on a site of Caves Inostranceva

222

1 1 1 1 2 DATA ACROSS LAKE LADOGA CONDUCTIVITY ANOMALY 1 1 2 1 1 2 Abstract

227

229

VELOCITIES FLOORS OF THE MANTLE UNDER FENNOSCANDIA ACCORDING TO SEISMOTOMOGRAPHY

z z z

II

. 2. The roof and the regions constant gradient on the of the mantle and transition zone the mantle

I I II

INTEGRO GIS INTEGRO AS A TOOL FOR COMPILATION OF COMPLEX GEOLOGICAL MODEL Abstract

. 1. of source data in 2 Scenes of GIS

1 2 1 2 BASIC MAGMATIC COMPLEXES OF THE VORONEZH CRYSTALLINE MASSIF AND ITS REFLECTION IN GEOPHYSICAL FIELDS 1 2 1 2

Ar 1-10 g a a g a 10

g a a g g

g g a g a g a a g a a g a a a a g a a

DEEP SEISMIC STUDIES IN THE SOUTHEASTERN FENNOSCANDIAN SHIELD

1 2 1 2

2

I I I

2 2

Structural scheme of Fennoscandian Shield

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

L Phoenix 2 0 T T 0 arg

L Phoenix L

L The resistivity curves and curves for registered of the for at a Ladoga

K

1 1 1 2 ELECTRICAL CONDUCTIVITY AS THE MANIFESTATION OF THE GEODYNAMIC PROCESSES IN THE GOLOVANIVSK SUTURE ZONE 1 A 1 1 2 Abstract rocks and metasomatic agneto methods in o the of the sedimentary rocks of the o and the o margin anomalies in Golovanivsk

270

271 11 11 11 17

272

MINERAGENIC AND RESOURCE POTENTIAL OF INDUSTRIAL MINERALS IN THE SWEKOFENNIAN PROVINCE (ADOPERATION) Abstract

277 2

Таблица 1 2 2 Al 2 Fe 2 Na 2 K 2 2. -

279 0

2

Таблица 2 >10 7 1 2

2 2 2

Fe 2

STUDY OF THE DEEP CONDUCTIVITY STRUCTURE OF THE 1 2 1 2 Summary Introduction 7 2

Applied technique Application in the ladoga project N and 21 Conclusions

1

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

291 References P

ELECTROMAGNETIC STUDY OF LITHOSPHERIC STRUCTURE OF MARGINAL ZONE OF THE EAST EUROPEAN CRATON IN NW POLAND Summary Introduction

The methods

Results

the largest singular values of the

297 Acknowledgments References

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 1 2 1 1 1 2 Summary Introduction Archean and early Proterozoic crystalline crust consists mainly of granites and

299 The methods

m has Results

1

Acknowledgments

References

THREE-DIMENSIONAL ELECTRICAL RESISTIVITY MODEL OF THE POMERANIA REGION IN NW POLAND ul. Summary goal task Introduction

study and include recently collected data The methods Results The resulting model of electrical resistivity ig

. Acknowledgments References

Res The conductivitystruc.

9 27 72 91 99

110 GI 172

292

CONTENT 9 27 Ivanov 72 91 99

110 Lavrov and 172

BASIC Shyrkov B I Burakhovych T K Kushnir A N

292

DEEP STRUCTURE AND GEODYNAMICS OF LAKE LADOGA REGION C 1