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Seismoacoustic research of lake bannoe bottom sediments (South Ural, Russia) of seismoacoustic surveying in the study of bottom sediments of Lake Bannoe, one of the lakes investigated as a part

SOME RESULTS OF RESEARCH SEISMOACOUSTIC USING PULSED SOURCE AND SEISMIC VIBRATION-MODULEResults of seismoacoustic researches with application of a pulse source and the vibrating

Physical Basis of Quasi-optimal Seismoacoustic Pulse Generating for Geophysical Prospecting in Shallow Water and Transit Zones. Part 2. The Layout of Aqueous Seismic Source and the Results of ExperimentsPhysical Basis of Quasi-optimal Seismoacoustic Pulse Generating for Geophysical Prospecting

USAGE OF NEW SEISMOACOUSTIC METHODS FOR PALEOLYMNOLOGICAL STUDY OF THE LADOGA AND ONEGA LAKESUSAGE OF NEW SEISMOACOUSTIC METHODS FOR PALEOLYMNOLOGICAL STUDY OF THE LADOGA AND ONEGA LAKES

METHODS OF CONDUCTING COMPLEX STUDIES TO RESTORE THE PALEOLIMOLOGICAL CONDITIONS AND UNDERWATER LANDSCAPES OF LARGE LAKES BY THE EXAMPLE OF PETROZAVODSK BAY OF LAKE ONEGA

Physical Basis of Quasi-optimal Seismoacoustic Pulse Generating for Geophysical Prospecting in Shallow Water and Transit Zones. Part 1. Theoretical foundationsPhysical Basis of Quasi-optimal Seismoacoustic Pulse Generating for Geophysical Prospecting

Climate changes over the last 13500 years based on lake sediments studies (Lake bolshoe Miassovo, South ural, Russia), Chelyabinsk region, Russia (55°9′59.89″N 60°20′51.82″E). Based on seismoacoustic investigation 5 long (up to 5

Выделение деструктивных зон в карбонатных венд-рифейских отложениях Восточной Сибири by variations of the seismo-acoustic properties and interpreted as local geological objects. The paper presents

PALEOLIMNOLOGY OF THE LARGEST EUROPEAN LAKES - LADOGA AND ONEGA

Micrometeorites from Lake Turgoyak, South Ural, Russia

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