Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine最新文献

{"title":"BASIC FOUNDATIONS OF THE METHODOLOGY OF STUDY OF THE INTERNAL STRUCTURE OF EARTH ACCORDING TO AEROSPACE SURVEY DATA","authors":"O. Azimov","doi":"10.30836/igs.2522-9753.2019.185752","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2019.185752","url":null,"abstract":"main foundations that are the basis of the methodology of investigation of the Earth crust structure using remote aerospace technologies are characterised conceptually from the phenomenological perspective. The keystone (first) principle con-cerns the knowledge of process for the simultaneous mutual interaction (paragenesis) of the physical forces oppositely direct-ed. These are the attractive power and the opposite of it the repulsive forces. The second principle is confined to determine of two groups for the geological driving forces (internal and external) for the appearance and evolution of the lithosphere structure. The third principle of remote sensing application for the geological purposes is based on the concept of existence both the plas-tic (quasiplastic) rock deformations and brittle (quasibrittle) ones. The fourth principle claims the existence of active processes for the permanent-interrupted energy-mass-exchange in the natural geosystems of the Planet as a manifestation of the special aspects for matter being and its forms of movements. The fifth principle states that the specific recent landscapes and the anomalies intrinsic to them as the geoindicators of interior structure of the geological substrate and energy-mass exchange processes connected with it are differentiated by the spectral features of reflected, absorbed, and emitted electromagnetic radi-ation in the different wave regions. As a result they are distinguished using these characteristics and may be imaged and iden-tified via remote sensing data.","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"86 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-11-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133638220","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"DEVELOPMENT OF VEGETATION AND SOILS IN THE CENTRAL PART OF THE PRYDNIPROVSKA UPLAND DURING THE SHYROKYNE AND MARTONOSHA STAGES OF THE EOPLEISTOCENE – EARLY NEOPLEISTOCENE","authors":"O. Sirenko, Zh.M. Matviishyna, Sergii P. Doroshkevych","doi":"10.30836/igs.2522-9753.2019.185744","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2019.185744","url":null,"abstract":"61 ВСТУП У тектонічному плані регіон досліджень відноситься до центральної частини Українського щита (УЩ) і згідно з районуванням четвертинних відкладів України розташований у позальодовиковій зоні. До недавнього часу відклади широкинського та мартоноського кліматолітів регіону досліджень палінологічно були практично не охарактеризовані. Узагальнена палінологічна характеристика широкинського кліматоліту отримана С.І. Турло за результатами вивчення розрізу біля с. Рожки Черкаської області (Турло, 1989). Графічно матеріали дослідження представлені у вигляді флористичної діаграми, на якій показано лише якісний склад пилку та спор і не зазначено кількісні показники. Мартоноські відклади досліджуваного регіону методом спорово-пилкового аналізу практично не вивчені. УДК (561:631.4):551.791(477) DOI:10.30836/igs.2522-9753.2019.185744","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"48 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-11-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128828504","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"RECONSTRUCTION OF CLIMATE OF PERIOD OF FORMATION OF AMBER-CONTAINING SEDIMENTS OF UKRAINIAN POLISSIA ON THE BASE OF PALYNOLOGICAL DATA BY COEXISTENCE APPROACH METHOD","authors":"Volodymyr Yu. Ochakovskyi","doi":"10.30836/igs.2522-9753.2019.185740","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2019.185740","url":null,"abstract":"Spore-pollen investigations of amber-bearing rocks of Ukrainian Polissia were conducted, two spore-pollen complexes were obtained. The taxonomic composition of both spore-pollen complexes is identical, they differ only in the proportions of the composition of the individual components: in the first SPC pollen of Pinaceae prevails over Taxodiaceae and Sciadopithys, angiosperm pollen is quite diverse, although its role is subordinate, in the second SPK pollen of Taxodiaceae and Sciadopithys prevails over Pinaceae, and the role of angiosperm pollen sharply decreases to several percent, a significant proportion of this group is Rhus pollen. On the base of own palynological investigation of amber-containing sediments of western Polissia a paleoclimate reconstruction of Mezhygorye time (early Oligocene) by coexistence approach (CA) method was done. The set of climate parameters has been expanded: mean annual temperature (MAT); mean temperature of the coldest month (CMT); mean temperature of the warmest month (WMT); mean annual precipitation (MAP); precipitation of the wettest month (HMP); precipitation of the direst month (LMP); precipitation of the warmest month (WMP).  Accuracy of calculation has been increased compared to previous studies. It is established that the climate was warm-temperate, narrow to subtropical (mean annual temperature +15,8°C). It corresponds to the modern climate of \"Csa\"-type according to the Koppen-Geiger classification (Mediterranean) or subtropical climate of the western coasts of the continents according to the Alisov classification.","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"13 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-11-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122100883","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Ukrainian lithology science: challenges and opportunities","authors":"E. Shnyukov, P. Gozhik, O. Mitropolskiy, S. Shekhunova","doi":"10.30836/igs.2522-9753.2018.150372","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2018.150372","url":null,"abstract":"","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130138968","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"ЛИТОЛОГИЧЕСКАЯ ХАРАКТЕРИСТИКА БАЛТСКИХ И САРМАТСКИХ ПЕСКОВ МЕЖДУРЕЧЬЯ САВРАНКИ И КОДЫМЫ КАК ВОЗМОЖНЫХ КОЛЛЕКТОРОВ НАКОПЛЕНИЯ ТЯЖЕЛЫХ МИНЕРАЛОВ","authors":"Natalya A. Fedoronchuk, I. A. Suchkov, Valentina O. Turbalak, Irina O. Goncharova, Ludmila Baranova","doi":"10.30836/igs.2522-9753.2018.150385","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2018.150385","url":null,"abstract":"The lithological composition of the Miocene-Pliocene sand deposits of the Middle Sarmatian and Baltian age between the rivers of the right tributaries of the Southern Bug (Savranka and Kodima rivers) was studied. Two series of sand are described in the composition of the Middle Sarmatian deposits. Under-limestone series has cross-bedding, which alternates with horizontal bedding. There are medium and coarse-grained sands with medium and good grading; there are layers of unsorted sandy-aleurite-clay material with a significant content of fine gravel. Garnet, magnetite, titanium-magnetite, ilmenite, rutile, glist predominate in the heavy fraction. Under-limestone series of the Middle Sarmatian is formed in coastal conditions with a flow hydrodynamic regime. Upper-limestone series of the Middle Sarmatian is composed of well-sorted medium-grained sands with an insignificant admixture of silt. The series is characterized by well-developed drift structure, expressed over tens of kilometers. The sands are enriched in heavy fraction, there are thin layers of black sand. Garnets, titanomagnetite, magnetite, ilmenite, rutile, glist predominate in the heavy fraction. Series is formed in the delta conditions that were established during the regression of the Sarmatian sea basin. The Baltian suite, which is the deposits of the Meotian, Pontian, Cimmerian and Akchagilian levels of the Miocene and Pliocene, was formed in continental conditions. The series is characterized by the alternation of aleurite-clay and sandy sediments, the presence of ironification, the wide distribution of clastogenic and authigenic postsedimentation carbon-bearing . The Baltian sands are predominantly fine-grained, sometimes clayey-silty, medium and well graded. Heavy minerals contain large quantities, among which ilmenite, titanium-magnetite, magnetite, garnet, zircon, and glist predominate. The Baltian suite was formed in the conditions of the alluvial plain that existed on the southern slope of the Ukrainian Shield in the Miocene-Pliocene. Compared to the Sarmatian deposits, Baltian sediments show a sharp increase in the amount of titanium-containing minerals and glists, this may be due to the erosion of new ore bodies with a decrease in the basis of erosion as a result of tectonic uplifting of the territory. The results of the study of the lithological composition and heavy fraction of Sarmatian and Baltian sandy sediments can be useful when searching for primary titanium-magnetite deposits, as well as when searching for alluvial placers on the right bank of the Southern Bug. In addition, such studies help in the reconstruction of alluvial pathways for the transfer of ore matter in the hypergenesis zone in the Northern Black Sea region.","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"42 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124291732","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"PALEOGEOGRAPHY FEATURES OF TOURNASIAN-VISEAN TIME OF THE AREA OF MECHEDIVSKO-SVIRIDIVSKA SADDLE AND ADJACENT TERRITORIES.","authors":"P. Korzhnev, Lyudmila I. Strуzhak, O. Naumenko, Tamara V. Husynina","doi":"10.30836/igs.2522-9753.2018.151526","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2018.151526","url":null,"abstract":"For detailing of Tournasian-Visean paleogeographic patterns of the north-western tectonic segment of the Dnipro-Donets depression data of quantitative spectral analysis of core samples have been used. Distribution of the groups of elements Ti, V, Mn, Ni, Co, Cr and Sr, Ba, Mn inside main lithological rocks types (sandstones-siltstones-argillites-carbonates) with taking into account factor of mono-minerality, are show the rate of intensity the physical/chemical weathering and allow to trace contours of catchments. The ratio Sr/Ba was used for definition of paleo-shore borders and delta-avandelta facies. Absorption of alkaline-earth elements (in particular Ba) from aqueous solutions in areas of mixing of saline and fresh waters is reflected in sporadic peak concentrations last ones in cement of sandstones and siltstones and, to a greater extent in higher background concentrations in argillites. Containing in solutions Ba were transported from feeding areas including as well magnetite ore fields of Voronezh anteclise, as evidenced by the established. Paleogeographic sketches were supplemented by analysis of textures by core samples and petrographic descriptions of thin sections. The conducted studies allowed to supplement and substantially elaborate the existing no-tions about the lithology and paleogeography of the north-western tectonic segment of the Dnipro-Donets depression during Tournasian-Visean. The alluvial plains on the territory of the axial and side parts of Dniprо-Donets depression were widely distributed in this time as well the presence of a desalinated sea basin on the territory of the Srebninska and Zhdanovska depressions has noted. Last one in particularly have been testified by presence of alluvial-delta and avandelta deposits of Mеchedivsko-Svуrуdivska saddle.","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"35 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117267103","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"GEOLOGICAL AND LITHOLOGICAL FEATURES OF THE LOWER PERMIAN SALT FORMATION OF THE JUNCTION ZONE OF THE DNIEPER-DONETS DEPRESSION AND THE NORTH-WESTERN DONBASS","authors":"M. V. Aleksieienkova","doi":"10.30836/igs.2522-9753.2018.152576","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2018.152576","url":null,"abstract":"COLLECTION OF SCIENTIFIC WORKS OF THE IGS NAS OF UKRAINE, VOL. 11, 2018 ВСТУП Незважаючи на тривалий період вивчення нижньопермської соленосної формації (понад три століття), залишається низка дискусійних питань щодо її стратиграфічного розчленування та геолого-літологічних особливостей. Крім того, протягом останніх десятиріч суттєво відрізнялися погляди і на тектонічне районування Дніпровсько-Донецької западини (ДДз), що також вносило свої корективи. Тому уточнення потребують не лише геолого-літологічні особливості, а й їх позиціювання відповідно до сучасного тектонічного районування. Зона зчленування південно-східної частини центрального грабена ДДз та північно-західного занурення Донецької складчастої споруди (Дсс) була виділена на південь від лінії ПавлоградКуп’янськ-Короча (Геология..., 1989) за низкою характеристик: зростанням потужності земної кори до 45 км, позитивними значеннями сили тяжіння з незначними широтними аномаліями, наявністю відкритих палеозойських структур північно-західного простягання та складної системи поперечних порушень (Геология..., 1989, Атлас... т.1, 1998; Дем’яненко, 2017). Згідно з сучасним тектонічним районуванням зона зчленування приурочена до тектонічних структур ІІ порядку: південно-східної центрикліналі осьової зони, перехідної (Близнюківсько-Шевченківського структурного вузла) й моноклінальної зон північної прибортової зони та моноклінальної (Близнюківська) й відкритої монокліналі південної прибортової зони Дніпровського грабену (Тектонічна..., 2007). Нижньопермська соленосна формація присутня лише в межах перехідної частини північної прибортової зони та у південно-східній центрикліналі. Наявність відкладів у межах моноклінальної зони північної прибортової зони прогнозоване, але не підтверджене даними буріння (Лапчук, 1990). Формація представлена двома субформаціями: соленосною (микитівська та слов’янська світи), стратиграфічне розчленування якої проводиться по маркуючих карбонатних горизонтах, та калієносно-магнієносною (краматорська світа), з стратиграфічним розчленуванням по ангідритових горизонтах (Кореневский и др., 1968; Шехунова, 2009). Нижня межа соленосної субформації (підошва микитівської світи) неузгоджена, та, за різними даними, проводиться по карбонатному горизонту R1 (Кореневский и др., 1968; Стратиграфія..., 2013), або (переважно в межах нафтогазових родовищ) – по карбонатному горизонту Q8 (Петлиця, Коломієць, 2009). Верхня межа микитівської світи умовно проводиться по підошві карбонатного горизонту S1, слов’янської світи – Т1 (белбасівський горизонт), краматорської світи – над пластом ангідриту аТ7 (Кореневский и др., УДК (553.631:553.776):504.062.2](477.6) DOI: https://doi.org/10.30836/igs.2522-9753.2018.153120","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"15 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121873859","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"THE UPPER VENDIAN TERRIGENOUS (PSAMMITIC) FORMATION OF PODILLIA","authors":"V. Grytsenko","doi":"10.30836/igs.2522-9753.2018.150882","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2018.150882","url":null,"abstract":"","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"103 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133533713","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"ANALYSIS OF KNOWLEDGE OF THE UPPER DEVONIAN SALT FORMATION IN THE SOUTHERN LATERAL PART OF THE PRIPYAT BASIN","authors":"N. P. Siumar","doi":"10.30836/IGS.2522-9753.2018.152982","DOIUrl":"https://doi.org/10.30836/IGS.2522-9753.2018.152982","url":null,"abstract":"A detailed study of the materials of previous research on the distribution of the Devonian deposits within the southern part of the Pripyat basin on the territory of Ukraine was carried out in order to determine their lithofacial composition. According to the results of the processing of the primary geological material (geological maps, sections and wells), modern distribution circuits of the Upper Devonian (Frasnian and Famennian) salt formations on the studied territory are established. The general description of the lithological composition of the Upper Devonian sediments is described and features of the material composition of salt formations are described. Perspectives of attraction of salt formations of this territory for use in underground construction are considered.","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134513793","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"THE BURIAL HISTORY OF PERMIAN SEDIMENTS IN THE CENTRAL PART OF THE DNIEPER-DONETS BASIN","authors":"I. Streltsova, I. Virshylo","doi":"10.30836/igs.2522-9753.2018.151466","DOIUrl":"https://doi.org/10.30836/igs.2522-9753.2018.151466","url":null,"abstract":"ЗБІРНИК НАУКОВИХ ПРАЦЬ ІНСТИТУТУ ГЕОЛОГІЧНИХ НАУК НАН УКРАЇНИ, ТОМ 11, 2018 INTRODUCTION Sedimentary basins studying require distinguishing not only dimensional distribution, but also the history of their transformation over geological time. Basin modeling is a crucial step in the regional and local hydrocarbon exploration. 1D simulation of the burial and thermal history includes all petroleum system elements. That is help to investigate sedimentary basins in detail. Today, petroleum geology has developed tools for evaluating the formation of a single УДК 551.8:553.981.2, (477.8) DOI: https://doi.org/10.30836/igs.2522-9753.2018.151466","PeriodicalId":191558,"journal":{"name":"Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine","volume":"7 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"116986156","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}