Goncharenko Olga Pavlovna
RussiaSaratovSaratov State University, 83, Astrakhanskaya Str., Saratov, 410012, Russiaprofessor, head of departmentDoctor of Geologo-Mineralogical SciencesGoncharenkoOP@mail.ru
Author's articles
- Depositional Environment in Bobrikovsky Time within the South-east of the Russian Plate
- Carnallite-halite Rocks and Halite of Gremyachinskoye Field’ Halogenous Formations and Their Role in Productive of Sylvinite Horizon Foundation
- On the Role of the Salting-out Processes at the Final Stages of Halogenesis (the Case of the Gremyachinskoye Potassium-Salt Field)
- Main Features of the Permian Halogenesis Hydrochemistry in the Caspian Region
- Terrigenous-mineralogic Characteristics of the Bobrikovskian Horizon from the Saratov Trans-Volga Region: Paleogeographical Aspects
- Sedimentation Model of the Upper Jurassic Productive Beds from the Southeast of the Yarsomovskij Site
- Reconstruction of the Late Vasyuganian Sedimentation Settings Within the Middle of Group of Fields
- Environment of Texture and Structure Formation in Potassium, Potassium-magnesium and Magnesium Salts within the Caspian Halogenic Basin
- Typomorphism of Clastogene Quartz from the «Melovatka-5» and «Melovatka-6» Sections (the Cenomanian from the Southeast of the Russian Plate)
- Peculiarities of Compositions and Formation Environments of Potassium and Potassium-Magnesium Rocks From the Pogozhskaya Rhythmic Member in The Northwestern and the Northeastern Parts of the Caspian Slope Zone
- In the Memory of Professor and Friend Konstantin Alekseevich Mavrin
- Features of Postsedimentation Alteration Sand Accessory Mineralization with in Rocks at Final Stages of Halogenesis in the Outer Slope Zone of the Caspian Depression
- Lithogeochemical Properties оf Terrigenous Rocks of Sortymsky Suite of Pyakyakhinskoye Field (North of Western Siberia)
- Paleogeographic and Tectonic Environment in the Lower Permian Halogen Formation from the Southeastern Margin of the Russian Plate
- Structural features of the lower permian salt-bearing series and the character of salt-tectogenesis manifestations in the northern and northwestern margins of the Сaspian depression. Paper 1
- Structural features of the lower Permian salt-bearing series and the character of salt-tectogenesis manifestations in the Caspian Depression. Paper II
- Insoluble remains of Lower Permian sylvinite rocks in the western and north-western framing of the Caspian depression