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Artykuły w czasopismach na temat „Geology, Stratigraphic Quaternary”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 29 lipca 2024

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1

Zolnikov, I. D., A. V. Shpansky, and M. V. Mikharevich. "PROBLEMS OF THE QUATERNARY STRATIGRAPHY OF THE SIBERIAN REGION." Geology and mineral resources of Siberia, no. 10s (December 2021): 3–6. http://dx.doi.org/10.20403/2078-0575-2021-10c-3-6.

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This special issue of the journal is devoted to modern controversial subjects arising during the research of the Siberian Quaternary system. The initiative to discuss these problems and new factual material that requires rethinking outdated stratigraphic constructions belonged to the section of the Quaternary system of SIBRMSK and was supported by leading experts actively working in the region. It should be noted that this issue does not cover all the unresolved issues on the geology, stratigraphy and paleogeography of the Quaternary period of Siberia.

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Shestopalov, Vyacheslav M., Oleksandr M. Ponomarenko, and Stella B. Shekhunova. "IN MEMORIAM OF PROFESSOR PETRO F. GOZHIK, ACADEMICIAN OF THE NATIONAL ACADEMY OF SCIENCES OF UKRAINE." Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine 14, no. 1 (May 20, 2021): 5–16. http://dx.doi.org/10.30836/igs.2522-9753.2021.232269.

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This article is devoted to the blessed memory of Petro F. Gozhik, prominent Ukrainian scientist in the fields of paleontology, stratigraphy, marine geology, Winner of the State Prizes of Ukraine in Science and Technology (1989, 2000), Merited Figure of Science and Technology of Ukraine (1997), Laureate of NAS Tutkovsky Prize (2008), Director of the Institute of Geological Sciences of the NAS of Ukraine (1997–2020), President of the Paleontological Society of Ukraine, Chairman of the National Stratigraphic Committee of Ukraine, initiator and the first Director of the National Antarctic Research

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Tian, Shaobing, Ping Zhang, Tongxiao Shang, Huogen Chen, Yongxiang Li, and Shugang Xu. "Application of resistivity sounding in Quaternary stratigraphic division in Yixing, Eastern China." Journal of Geophysics and Engineering 19, no. 3 (June 1, 2022): 362–75. http://dx.doi.org/10.1093/jge/gxac025.

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Abstract Stratigraphic classification and correlation are fundamental for the study of regional geology, tectonic structures and paleogeographic evolution. Geological structures have undergone a dramatic change since the Quaternary. However, the division of the Quaternary stratigraphic boundary in southeastern China is debated. In this study, we used a direct current vertical electric sounding method to study the Quaternary strata in Yixing, Jiangsu, China. Using one-dimensional resistivity inversion and analyzing the regional geology and geological core data, the electrical features of the st

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4

Slupik, A. A., F. P. Wesselingh, A. C. Janse, and J. W. F. Reumer. "The stratigraphy of the Neogene-Quaternary succession in the southwest Netherlands from the Schelphoek borehole (42G4-11/42G0022) – a sequence-stratigraphic approach." Netherlands Journal of Geosciences - Geologie en Mijnbouw 86, no. 4 (December 2007): 317–32. http://dx.doi.org/10.1017/s0016774600023556.

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AbstractWe investigate the stratigraphy of Neogene and Quaternary intervals of the Schelphoek borehole (Schouwen, Zeeland, the Netherlands). The Breda Formation (Miocene-Zanclean) contains three sequences separated by hiatuses. The Oosterhout Formation (Zanclean-Piacenzian) contains at least two sequences. This formation is overlain by seven sequences of the Gelasian Maassluis Formation that almost certainly represent glacial cycles. The three lowermost sequences are provisionally assigned to the Praetiglian (MIS 96, MIS 98 and MIS 100). A large hiatus exists between the top of the Maassluis F

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5

Josenhans, H. W., J. Zevenhuizen, and R. A. Klassen. "The Quaternary geology of the Labrador Shelf." Canadian Journal of Earth Sciences 23, no. 8 (August 1, 1986): 1190–213. http://dx.doi.org/10.1139/e86-116.

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The regional distribution of glacial and postglacial sediments on the Labrador Shelf was mapped by medium- and high-resolution seismics and shows a succession of tills that extend to the continental shelf edge at approximately 600 m. The uppermost of these tills is less laterally extensive and does not occur on the Labrador Shelf bank tops in water depths less than 160 m. We infer that the last glacial episode was less extensive than the preceding ones. Glaciomarine stratified silts and postglacial muds are found overlying the upper till in the deep basins that separate the banks. The upper ti

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6

Long, Joshua H., Till J. J. Hanebuth, and Thomas Lüdmann. "The Quaternary stratigraphic architecture of a low-accommodation, passive-margin continental shelf (Santee Delta region, South Carolina, U.S.A.)." Journal of Sedimentary Research 90, no. 11 (November 30, 2020): 1549–71. http://dx.doi.org/10.2110/jsr.2020.006.

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ABSTRACT The Quaternary stratigraphy of the continental shelf offshore of South Carolina consists of stratigraphic units deposited in coastal-plain, shallow marine, and shelfal environments bounded by composite erosional surfaces that developed in response to numerous glacioeustatic cycles and were overprinted by regional uplift. These units are commonly distributed laterally, rather than stacked vertically, a function of the long-term low shelf gradient and the resulting lack of accommodation. Additionally, marine processes such as waves and geostrophic currents can rework both relict and mod

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Cooper, A. J. "Waste disposal site selection techniques in Quaternary terraine Ontario, Canada." Geological Society, London, Engineering Geology Special Publications 7, no. 1 (1991): 211–17. http://dx.doi.org/10.1144/gsl.eng.1991.007.01.19.

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AbstractThick and predictable deposits of fine grained Quaternary materials have been used for the siting of waste management facilities in Ontario. The search for such sites is founded on the application of techniques in Quaternary geology and hydrogeology. Two examples are presented. Oxford County is located southwest of Toronto in an area of parallel morainic ridges separated by flat till plains. Conventional wisdom would focus on the till plains for thick, consistent fine grained Quaternary Sediments. However, the careful analysis of the Quaternary stratigraphy and glacial history revealed

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8

Aiello, Gemma, and Mauro Caccavale. "Quaternary Evolution of Ischia: A Review of Volcanology and Geology." Applied Sciences 13, no. 6 (March 10, 2023): 3554. http://dx.doi.org/10.3390/app13063554.

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Ischia shows intriguing and complex geology, which has been deeply investigated. In this paper, a reappraisal of the Quaternary geologic evolution of Ischia based on literature data is advised, concentrating on the volcanology of the island, based on field data and geochemistry, due to the happening of active fumarolic systems on the island and the marine geology and geophysics, which are intensively studied in the frame of the CARG Project. The literature studies have been incorporated with the geological interpretation of high-resolution seismic profiles, partly previously published and here

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9

Gaudenyi, Tivadar, Drazenko Nenadic, Mladjen Jovanovic, and Petar Stejic. "The revision of quaternary stratigraphy of the Zrenjanin artesian well borehole profile (Banat, Vojvodina, Serbia)." Annales g?ologiques de la Peninsule balkanique, no. 00 (2022): 7. http://dx.doi.org/10.2298/gabp210306007g.

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The geological analysis of artesian borehole material from Sombor, Subotica, and Zrenjanin, was in the first campaign of detailed stratigraphic studies of Vojvodina in 1892-1895. The results of Quaternary stratigraphy from Zrenjanin were published by HalavAts m ore than a decade later (1914). The significance of the Zrenjanin, Sombor, and Subotica artesian well profiles for more than a century is considered the representative local profiles for the Quaternary stratigraphy of Vojvodina recognized by Serbian (Yugoslavian) and Hungarian geologists. Significant changes were after the taxonomical r

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10

Amos, Salvador. "A stable Cenozoic geologic time scale is indispensable." GeoArabia 11, no. 4 (October 1, 2006): 155–57. http://dx.doi.org/10.2113/geoarabia1104155.

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A stable, standard geologic time scale is indispensable for the clear and precise communication among geologists; it is a basic tool of geologic work. Considerable progress has been made to achieve such a stable time scale. However, during the last few years several proposals have been made to modify the Cenozoic section of the geologic time scale that threaten to destabilize it. Seven articles published in Episodes since 2000 that could contribute to this destabilization are discussed. They provide excellent examples of the profusion of different terminologies, hierarchies, and stratigraphic

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11

Hinojosa-Prieto, Hector R., Pantelis Soupios, and Pavel Barsukov. "Subsurface Geological Characterization of the Late Neogene–Quaternary Argive Basin, Peloponnese, Greece Using Transient Electromagnetic Data and Vintage Stratigraphic Logs." Geosciences 11, no. 8 (July 28, 2021): 317. http://dx.doi.org/10.3390/geosciences11080317.

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The onshore and offshore clastic deposits of the Argive Basin and the Argolic Gulf, respectively, in Peloponnese, Greece, form a Late Neogene–Quaternary half-graben that connects with the Aegean Sea. The onshore Late Neogene–Quaternary sequence, comprised of chaotically intercalated cohesive and granular clastic deposits, is in angular unconformity with bedrock comprised of Triassic–Upper Cretaceous strongly-weathered, highly-fractured karstic limestones thrusted against Paleogene flysch deposits. While the surface geology of the Argive Basin is well-known, the subsurface geology remains both

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12

Munsterman, D. K., R. M. C. H. Verreussel, H. F. Mijnlieff, N. Witmans, S. Kerstholt-Boegehold, and O. A. Abbink. "Revision and update of the Callovian-Ryazanian Stratigraphic Nomenclature in the northern Dutch offshore, i.e. Central Graben Subgroup and Scruff Group." Netherlands Journal of Geosciences - Geologie en Mijnbouw 91, no. 4 (December 2012): 555–90. http://dx.doi.org/10.1017/s001677460000038x.

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AbstractExploration in a mature basin requires a detailed classification and standardisation of rock stratigraphy to adequately comprehend the depositional history and prospect architecture. The pre-Quaternary Stratigraphic Nomenclature of the Netherlands compiled by Van Adrichem Boogaert & Kouwe in 1993 provided a consistent framework for use by the Dutch geological community. Over the past twenty years, new biostratigraphic techniques and continued exploration in the Netherlands have provided additional stratigraphic information. Based on this information the Late Jurassic lithostratigra

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13

Corrado, Giuseppe, Sabrina Amodio, Pietro P. C. Aucelli, Gerardo Pappone, and Marcello Schiattarella. "The Subsurface Geology and Landscape Evolution of the Volturno Coastal Plain, Italy: Interplay between Tectonics and Sea-Level Changes during the Quaternary." Water 12, no. 12 (December 2, 2020): 3386. http://dx.doi.org/10.3390/w12123386.

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The Volturno alluvial-coastal plain is a relevant feature of the Tyrrhenian side of southern Italy. Its plan-view squared shape is due to Pliocene-Quaternary block-faulting of the western flank of the south-Apennines chain. On the basis of the stratigraphic analysis of almost 700 borehole logs and new geomorphological survey, an accurate paleoenvironmental reconstruction before and after the Campania Ignimbrite (CI; about 40 ky) eruption is here presented. Tectonics and eustatic forcing have been both taken into account to completely picture the evolution of the coastal plain during Late Quate

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14

Reichenbacher, Renee, Roy Van Arsdale, Randel Cox, and Chris Cramer. "Geomorphology, Three-Dimensional Geology, and Seismologic Hazards of the New Madrid Seismic Zone in Dyer County, Tennessee." Environmental & Engineering Geoscience 28, no. 2 (April 22, 2022): 147–71. http://dx.doi.org/10.2113/eeg-d-21-00005.

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ABSTRACT Geomorphic and three-dimensional geologic mapping reveals two major fault systems of the seismically active Reelfoot rift pass beneath Dyer County in northwestern Tennessee, the Reelfoot South fault, and the east-bounding faults of the Reelfoot rift. The Dyer County mapping also indicates that the two principal Reelfoot South fault hanging wall structures, the Lake County uplift and Tiptonville dome, pass beneath the county. Quaternary displacement was identified on southeastern Reelfoot rift margin faults in Dyer County, thus indicating that this rift margin has been active during th

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15

Kosters, Elisabeth C., Bart E. J. M. VanMierlo, Nico H. Verbeek, Bart J. Posthumus, Thomas M. McGee, and Jan Brouwer. "Late Quaternary stratigraphic signature, offshore from the Dutch barrier shoreline." Sedimentary Geology 80, no. 3-4 (October 1992): 199–212. http://dx.doi.org/10.1016/0037-0738(92)90041-o.

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Novianto, Ardian, Sutanto, Suharsono, Carolus Prasetyadi, and Jatmiko Setiawan. "Structure Boundary Separating using Gravity Data for Central and Southern Parts of the East Java Basin Beneath the Quaternary Volcanic Deposits." Iraqi Geological Journal 55, no. 1B (February 28, 2022): 1–13. http://dx.doi.org/10.46717/igj.55.1b.1ms-2022-02-17.

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Stratigraphic interpretation shows that the relationship between Cenozoic volcanic rocks deposited in the Southern Mountains and marine clastic volcanic rocks in the Kendeng Basin possibly forms a stratigraphic transition bordered by the major fault that is yet to be defined. The thick Quaternary volcanic deposits obstruct field observation on the surface. Miocene outcrops in limited presence are found on the volcanic slope, positioned relatively more to the north than the same outcrop. This feature indicates major thrusting in southern Java that moved it to the north. The gravity data analysi

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17

Amador, Elmo Da Silva. "Geologia e Geomorfologia da Planície Costeira da Praia do Sul: Ilha Grande - Uma Contribuição à Elaboração do Plano Diretor da Reserva Biológica." Anuário do Instituto de Geociências 11 (January 1, 1987): 35–58. http://dx.doi.org/10.11137/1987_0_35-58.

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Based on stratigraphical, sedimentological and geomorphological methods, a preliminary stratigraphic division is proposed to the Praia do Sul coastal plain, a state Biological Reserve, located in "Ilha Grande", Rio de Janeiro. This reserve was created to preserve the natural ecosystems found therein (sandy coastal plain, mangrove, lagoon, rocky coast and hillside fo rest). The Praia do Sul sedimentation plain is essentially constituted by continental gravels and sands of Upper Pleistocene, marine sandy formations, fluvial-lagoonal sandy-clayer formations and present mangrove swamps and beachs.

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18

Iannace, Pietro, Maurizio M. Torrente, and Alfonsa Milia. "Tectono-stratigraphic evolution of the Southern Campania Margin: a key area for the evolution of the Tyrrhenian-Apennine system." Oil & Gas Science and Technology – Revue d’IFP Energies nouvelles 73 (2018): 39. http://dx.doi.org/10.2516/ogst/2018035.

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The Southern Campania Margin (SCM) represents a key area of the Central Mediterranean because it records all the rifting stages of the Tyrrhenian Sea. The interpretation of a seismic dataset calibrated with deep wells and outcrops, using seismic stratigraphy and structural geology methods in a dedicated Geographic Information System (GIS) environment, the seismic depth conversion, the generation of 2-D and 3-D models led to the reconstruction of a polyphased tectono-stratigraphic evolution of the SCM. During the early stage of Tyrrhenian opening a terrigenous transtensional Basin (Langhian-Tor

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19

Dongol, Gopal M. S. "The stratigraphic significance of vertebrate fossils from the Quaternary deposits of the Kathmandu Basin, Nepal." Newsletters on Stratigraphy 18, no. 1 (October 28, 1987): 21–29. http://dx.doi.org/10.1127/nos/18/1987/21.

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Mikharevich, M. V., and A. V. Shpansky. "PROBLEMS OF AGE AND GENETIC DIAGNOSTICS OF QUATERNARY DEPOSITS IN THE VALLEY OF THE YENISEI RIVER MIDDLE COURSE (YENISEI – LOWER ANGARA STRATIGRAPHIC REGION AND THE MINUSINSK BASINS AREA)." Geology and mineral resources of Siberia, no. 10s (December 2021): 57–68. http://dx.doi.org/10.20403/2078-0575-2021-10c-57-68.

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The article is devoted to the state of stratigraphic exploration maturity of the Eopleistocene – Neo-Рleistocene Quaternary deposits on the boundary of mountain and plain territories in the non-glacial area. The material analysis shows an inadequate rationale of the existing stratigraphic schemes, according to which the ladder of alluvial terraces of these territories was formed sequentially during the Eopleistocene, Neo-Pleistocene and Holocene. The revising of representative sections was carried out, the provision of them with geochronological data, the accuracy of age and genetic diagnostic

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21

Weijermars, Ruud. "Surface Geology, Lithostratigraphy and Tertiary Growth of the Dammam Dome, Saudi Arabia: A New Field Guide." GeoArabia 4, no. 2 (April 1, 1999): 199–226. http://dx.doi.org/10.2113/geoarabia0402199.

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ABSTRACT The surface geology of the Dammam Dome, Saudi Arabia, is documented in the geographic context of the modern and extensive urban and industrial developments in this area. A new geologic road map shows where key Tertiary outcrops occur relative to major roads, and columnar sections and field photographs illustrate the stratigraphic relationships and support the discussion on depositional environments. Surface geology is also used to infer growth rates for the Dammam field. These rates are generally consistent with those determined from subsurface data in the Awali field. The Dammam Dome

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22

Leroux, Estelle, Marina Rabineau, Daniel Aslanian, Christian Gorini, François Bache, Maryline Moulin, Romain Pellen, Didier Granjeon, and Jean-Loup Rubino. "Post-rift evolution of the Gulf of Lion margin tested by stratigraphic modelling." Bulletin de la Société Géologique de France 186, no. 4-5 (July 1, 2015): 291–308. http://dx.doi.org/10.2113/gssgfbull.186.4-5.291.

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AbstractThe sedimentary architecture of basins and passive margins is determined by a complex interaction of parameters, including subsidence, eustasy, and sediment supply. A quantification of the post-rift (20 Ma-0 Ma) vertical movements of the Gulf of Lion (West Mediterranean) is proposed here based on the stratigraphic study of sedimentary paleomarkers using a large 3D grid of reflection seismic data, correlations with existing drillings, and refraction data. Post-rift subsidence was measured by the direct use of sedimentary geometries analysed in 3D and validated by numerical stratigraphic

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23

Cianflone, Giuseppe, Giuseppe Cavuoto, Michele Punzo, Rocco Dominici, Maurizio Sonnino, Vincenzo Di Fiore, Nicola Pelosi, et al. "Late quaternary stratigraphic setting of the Sibari Plain (southern Italy): Hydrogeological implications." Marine and Petroleum Geology 97 (November 2018): 422–36. http://dx.doi.org/10.1016/j.marpetgeo.2018.07.027.

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Bullejos, Manuel, David Cabezas, Manuel Martín-Martín, and Francisco Javier Alcalá. "A K-Nearest Neighbors Algorithm in Python for Visualizing the 3D Stratigraphic Architecture of the Llobregat River Delta in NE Spain." Journal of Marine Science and Engineering 10, no. 7 (July 19, 2022): 986. http://dx.doi.org/10.3390/jmse10070986.

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The k-nearest neighbors (KNN) algorithm is a non-parametric supervised machine learning classifier; which uses proximity and similarity to make classifications or predictions about the grouping of an individual data point. This ability makes the KNN algorithm ideal for classifying datasets of geological variables and parameters prior to 3D visualization. This paper introduces a machine learning KNN algorithm and Python libraries for visualizing the 3D stratigraphic architecture of sedimentary porous media in the Quaternary onshore Llobregat River Delta (LRD) in northeastern Spain. A first HTML

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Bogucki, Andriy, Zhanna Matviishyna, Olena Tomeniuk, and Serhii Doroshkevych. "IN MEMORIAM OF ACADEMICIAN PETRO GOZHYK – THE OUTSTANDING RESEARCHER OF THE QUATERNARY AND ORGANIZER OF SCIENCE." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 15 (September 25, 2023): 20–29. http://dx.doi.org/10.30970/gpc.2023.1.3945.

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Academician Petro Feodosiyovych Gozhyk is a prominent Ukrainian geologist, palaeontologist, palaeogeographer and researcher of the Quaternary. All his scientific activity was related to the Institute of Geological Sciences of the National Academy of Sciences of Ukraine, in which he worked his way up from graduate student to the director position. The scientific interests of the researcher cover a wide range of Earth sciences – from the study of molluscs to marine geology and Antarctic research. The publication presents the main milestones of Petro Gozhyk's life and scientific and organizationa

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Filipovich, Rubén, Walter Báez, Gianluca Groppelli, Florencia Ahumada, Luca Aldega, Raúl Becchio, Gabriele Berardi, et al. "Geological Map of the Tocomar Basin (Puna Plateau, NW Argentina). Implication for the Geothermal System Investigation." Energies 13, no. 20 (October 20, 2020): 5492. http://dx.doi.org/10.3390/en13205492.

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This paper presents a detailed geological map at the 1:20,000 scale of the Tocomar basin in the Central Puna (north-western Argentina), which extends over an area of about 80 km2 and displays the spatial distribution of the Quaternary deposits and the structures that cover the Ordovician basement and the Tertiary sedimentary and volcanic units. The new dataset includes litho-facies descriptions, stratigraphic and structural data and new 234U/230Th ages for travertine rocks. The new reconstructed stratigraphic framework, along with the structural analysis, has revealed the complex evolution of

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Onnis, Luciano, Roberto Antonio Violante, Ana Osella, Matías De la Vega, Alejandro Tassone, and Ernesto López. "Neogene-Quaternary seismic stratigraphy of the Llancanelo Lake Basin, Mendoza, Argentina." Andean Geology 45, no. 1 (November 14, 2017): 35. http://dx.doi.org/10.5027/andgeov45n1-3026.

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A new shallow multichannel seismic survey was carried out in the Llancanelo Lake region (Southern Mendoza Province, Argentina), in order to complete and extend previously surveyed seismic sections. The new seismic data allowed to double the already existing data. The obtained information was correlated with seismic and stratigraphic data from the industry. In this way it was possible to depict the major Neogene-Quaternary sedimentary-volcanic sequences and the regional evolution of a tectonic-volcanic basin located in a key region at the eastern foot of the Andes cordillera. This research is s

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Dohrenwend, J. C., S. G. Wells, and L. D. McFadden. "Geomorphic and stratigraphic indicators of Neogene-Quaternary climatic change in arid and semiarid environments." Geology 14, no. 3 (1986): 263. http://dx.doi.org/10.1130/0091-7613(1986)14<263:gasion>2.0.co;2.

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Sincavage, Ryan, Paul M. Betka, Stuart N. Thomson, Leonardo Seeber, Michael Steckler, and C. Zoramthara. "Neogene shallow-marine and fluvial sediment dispersal, burial, and exhumation in the ancestral Brahmaputra delta: Indo-Burman Ranges, India." Journal of Sedimentary Research 90, no. 9 (September 1, 2020): 1244–63. http://dx.doi.org/10.2110/jsr.2020.60.

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ABSTRACT The stratigraphic record of Cenozoic uplift and denudation of the Himalayas is distributed across its peripheral foreland basins, as well as in the sediments of the Ganges–Brahmaputra Delta (GBD) and the Bengal–Nicobar Fan (BNF). Recent interrogation of Miocene–Quaternary sediments of the GBD and BNF advance our knowledge of Himalayan sediment dispersal and its relationship to regional tectonics and climate, but these studies are limited to IODP boreholes from the BNF (IODP 354 and 362, 2015-16) and Quaternary sediment cores from the GBD (NSF-PIRE: Life on a tectonically active delta,

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Gentili, Bernardino, Gilberto Pambianchi, Domenico Aringoli, Marco Materazzi, and Marco Giacopetti. "Pliocene –Pleistocene geomorphological evolution of the Adriatic side of Central Italy." Geologica Carpathica 68, no. 1 (February 1, 2017): 6–18. http://dx.doi.org/10.1515/geoca-2017-0001.

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Abstract This work is a significant contribution to knowledge of the Quaternary and pre-Quaternary morphogenesis of a wide sector of central Italy, from the Apennine chain to the Adriatic Sea. The goal is achieved through a careful analysis and interpretation of stratigraphic and tectonic data relating to marine and continental sediments and, mostly, through the study of relict limbs of ancient landscapes (erosional surfaces shaped by prevailing planation processes). The most important scientific datum is the definition of the time span in which the modelling of the oldest morphological elemen

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Cerdeño, Esperanza, Natalia P. Lucero, and Jorge O. Chiesa. "Quaternary Mammals from Central-Western Argentina in the Stratigraphic Context of Southern South America." Quaternary 6, no. 4 (December 4, 2023): 59. http://dx.doi.org/10.3390/quat6040059.

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This is an updated contribution to the Quaternary geology and paleontology from central-western Argentina, focused on San Luis Province. It is mostly based on unpublished data; only some fossils had previously been briefly mentioned in broader faunal contexts. The fossil-bearing sediments correspond to eolian and alluvial environments of moderate energy, dominated by sands and sandy silts. They overlie high-energy fluvial cycles and underlie edaphic horizons. They have a wide distribution, and several radiocarbon dates allow their regional correlation. Stratigraphic sequences with the precise

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Zembo, Irene. "Stratigraphic architecture and quaternary evolution of the Val d'Agri intermontane basin (Southern Apennines, Italy)." Sedimentary Geology 223, no. 3-4 (January 2010): 206–34. http://dx.doi.org/10.1016/j.sedgeo.2009.11.011.

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Bowman, Steven A. "Regional seismic interpretation of the hydrocarbon prospectivity of offshore Syria." GeoArabia 16, no. 3 (July 1, 2011): 95–124. http://dx.doi.org/10.2113/geoarabia160395.

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ABSTRACT Analysis of 5,000 km of multi-client long-offset 2-D seismic data has led to the identification of three sedimentary basins, Levantine, Cyprus, and Latakia, located in offshore Syria. Each basin has a unique structural and stratigraphic history. They are separated from each other by the middle to Late Cretaceous aged Latakia Ridge System that initiated as a compressional fold-thrust belt and was re-activated under a sinistral strike-slip regime that developed during the Early Pliocene in response to a re-organisation of the plate-tectonic stresses. There is significant evidence for a

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Ward, Dylan J. "Dip, layer spacing, and incision rate controls on the formation of strike valleys, cuestas, and cliffbands in heterogeneous stratigraphy." Lithosphere 11, no. 5 (August 2, 2019): 697–707. http://dx.doi.org/10.1130/l1056.1.

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Abstract Landscapes developed over heterogeneous stratigraphy exhibit a spectrum of landforms from dramatic cliffbands to hogbacks, depending on the dip and spacing of the layers. In deeply incised landscapes, a single cliffband may consist of multiple resistant layers, whereas similar stratigraphy elsewhere is separated by strike valleys into individual cuesta benches or hogbacks. This paper presents a geometric analysis, informed by a numerical landscape model, to explain the conditions for development of a strike valley floored by erodible rocks. The results define a threshold incision rate

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Costa, Mario, Jessica Chicco, Chiara Invernizzi, Simone Teloni, and Pietro Paolo Pierantoni. "Plio–Quaternary Structural Evolution of the Outer Sector of the Marche Apennines South of the Conero Promontory, Italy." Geosciences 11, no. 5 (April 24, 2021): 184. http://dx.doi.org/10.3390/geosciences11050184.

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Some new results and preliminary remarks about the Plio–Quaternary structural and evolutionary characteristics of the outer Marche Apennines south in the Conero promontory are presented in this study. The present analysis is based on several subsurface seismic reflection profiles and well data, kindly provided by ENI S.p.A. and available on the VIDEPI list, together with surface geologic–stratigraphic knowledge of Plio–Quaternary evolution from the literature. Examples of negative vs. positive reactivation of inherited structures in fold and thrust belts are highlighted. Here, we present an ex

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Wang, Zhongbo, Shouye Yang, Qiang Wang, Zhixun Zhang, Xunhua Zhang, Xianhong Lan, Rihui Li, and Long Huang. "Late Quaternary stratigraphic evolution on the outer shelf of the East China Sea." Continental Shelf Research 90 (November 2014): 5–16. http://dx.doi.org/10.1016/j.csr.2014.04.015.

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Waters, Michael R., Steven L. Forman, and James M. Pierson. "Late Quaternary Geology and Geochronology of Diring Yuriakh, An Early Paleolithic Site in Central Siberia." Quaternary Research 51, no. 2 (March 1999): 195–211. http://dx.doi.org/10.1006/qres.1998.2024.

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AbstractDiring Yuriakh, an archaeological site on the highest terrace of the Lena River in subarctic eastern Siberia, provides evidence for the oldest and northern-most Early Paleolithic occupation in Asia. Stratigraphic and sedimentological studies at the site show that artifacts occur on a single eolian deflation surface that is underlain by fluvial sediments with inset cryogenic sand wedges and overlain by eolian deposits. Thermoluminescence ages on the fine-grained extracts from the eolian sediments and sand wedges that bound the artifact level indicate that the occupation occurred >260

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Elsheikh, Mahmoud. "Seismic Stratigraphic Analysis and Hydrocarbon Potential of Miocene-Quaternary Deposits in the Western Nile Delta Basin." Iraqi Geological Journal 54, no. 2C (September 30, 2021): 1–12. http://dx.doi.org/10.46717/igj.54.2c.1ms-2021-09-20.

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This study focuses on the subsurface Miocene-Pleistocene sedimentary sequence of the Western Delta of Deep-Sea field. Analysis of seismic, based on obtainable well data, and seismic data, allows us to divide the studied successions into two mega sequences: Pre and Post Messinian complexes resulting in transgressive-regressive sedimentation cycles of sea level during the evolution of the Miocene-Pleistocene subsurface sedimentary sequence. The Relative level of the sea was extremely falling in the time of the Messinian period, although it was largely rising at the time of the lower to Middle Pl

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Parsons, B., D. J. P. Swift, and K. Williams. "Quaternary Facies Assemblages and Their Bounding Surfaces, Chesapeake Bay Mouth: An Approach to Mesoscale Stratigraphic Analysis." Journal of Sedimentary Research 73, no. 5 (September 1, 2003): 672–90. http://dx.doi.org/10.1306/012103730672.

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Mycielska-Dowgiałło, E., and B. Woronko. "The degree of aeolization of Quaternary deposits in Poland as a tool for stratigraphic interpretation." Sedimentary Geology 168, no. 3-4 (June 2004): 149–63. http://dx.doi.org/10.1016/j.sedgeo.2003.12.006.

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Li, Congxian, Ping Wang, Heping Sun, Jiaqiang Zhang, Daidu Fan, and Bing Deng. "Late Quaternary incised-valley fill of the Yangtze delta (China): its stratigraphic framework and evolution." Sedimentary Geology 152, no. 1-2 (September 2002): 133–58. http://dx.doi.org/10.1016/s0037-0738(02)00066-0.

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Collier, R. E. Ll, M. R. Leeder, and J. R. Maynard. "Transgressions and regressions: a model for the influence of tectonic subsidence, deposition and eustasy, with application to Quaternary and Carboniferous examples." Geological Magazine 127, no. 2 (March 1990): 117–28. http://dx.doi.org/10.1017/s0016756800013819.

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AbstractThe position of a coastline in time and space is determined by (1) the vertical displacement and/or tilting of the depositional surface, (2) the rate of sediment accumulation or erosion across that surface, and (3) variation of sea-level. All three rates of change may vary through time. We present computer simulations of coastline movements that illustrate the interaction of the above variables, with (1) and (2) held at various defined levels whilst (3) is varied according to the late Quaternary glacio-eustatic sea-level curve. The Corinth Canal section in central Greece exposes uplift

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Krapivner, Rudol'f Borisovich. "The problem of genesis of quaternary deposits of the Barents Sea as a reflection of the overall crisis of glacial theory." Арктика и Антарктика, no. 4 (April 2020): 80–102. http://dx.doi.org/10.7256/2453-8922.2020.4.34164.

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This article continues the discussion on quaternary geology and paleogeography of the vast and well-studied shelf of the Barents Sea. The object this research is the relief and quaternary formations of the Barents shelf. The data of seismic-acoustic profiling and materials of engineering-geological drilling were used. Since the Barents shelf is a high-latitude area of Holocene sedimentation, the author analyzes various aspects of the quaternary sediments genesis, taking into account the geographic zoning of marine sedimentation processes and an increase in the gravitational consolidation of se

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Hearty, Paul J., and Darrell S. Kaufman. "Whole-Rock Aminostratigraphy and Quaternary Sea-Level History of the Bahamas." Quaternary Research 54, no. 2 (September 2000): 163–73. http://dx.doi.org/10.1006/qres.2000.2164.

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The surficial geology of the tectonically stable Bahamian archipelago preserves one of the most complete records of middle to late Quaternary sea-level-highstand cycles in the world. However, with the exception of deposits from marine isotope substage (MIS) 5e, fossil corals for radiometric dating of this rich stratigraphic sequence are rare. This study utilizes the previously published, independent lithostratigraphic framework as a testing ground for amino acid racemization in whole-rock limestone samples. At least six limestone–soil couplets provide a relative age sequence of events that enc

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Larsen, B., and L. T. Andersen. "Late Quaternary stratigraphy and morphogenesis in the Danish eastern North Sea and its relation to onshore geology." Netherlands Journal of Geosciences 84, no. 2 (July 2005): 113–28. http://dx.doi.org/10.1017/s0016774600023003.

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AbstractGeological structures and Late Quaternary stratigraphy of the shallow subsurface along the southernmost Danish North Sea coast have been investigated using seismic data and shallow boreholes. A large-scale glaciotectonic thrust complex has been mapped in an area of 15 km by 40 km in the Fanø Bugt area. The affected succession consists of Neogene and Quaternary sediments deformed down to a depth of 200 – 360 m. A kineto-stratigraphic correlation to onshore glaciotectonic deformation suggests that the deformation took place during a westward advance stage of the Late Saalian (Warthe) gla

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Japsen, Peter, and Torben Bidstrup. "Quantification of late Cenozoic erosion in Denmark based on sonic data and basin modelling." Bulletin of the Geological Society of Denmark 46 (December 20, 1999): 79–99. http://dx.doi.org/10.37570/bgsd-1999-46-08.

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The amount of section missing because of late Cenozoic erosion is estimated using basin modelling and sonic data from four stratigraphic levels in 68 Danish wells, and is found to be smaller than estimated in previous studies. The missing section increases from zero in the western and southern part of the Danish North Sea to 1000–1200 m towards north-east, on and along the Skagerrak-Kattegat Platform. In a broad intermediate zone, c. 500 m of mainly Paleocene–Miocene sediments are missing where Paleocene sediments subcrop the Quaternary. On the Skagerrak-Kattegat Platform, an additional c. 500

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Mancini, Marco, Gianluca Vignaroli, Francesco Bucci, Mauro Cardinali, Gian Paolo Cavinato, Cristina Di salvo, Silvia Giallini, et al. "New stratigraphic constraints for the Quaternary source‐to‐sink history of the Amatrice Basin (central Apennines, Italy)." Geological Journal 55, no. 6 (November 3, 2019): 4226–51. http://dx.doi.org/10.1002/gj.3672.

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Busson, J., P. Joseph, T. Mulder, V. Teles, J. Borgomano, D. Granjeon, C. Betzler, E. Poli, and M. Wunsch. "High-resolution stratigraphic forward modeling of a Quaternary carbonate margin: Controls and dynamic of the progradation." Sedimentary Geology 379 (January 2019): 77–96. http://dx.doi.org/10.1016/j.sedgeo.2018.11.004.

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KRÖCHERT, JÖRG, and ELMAR BUCHNER. "Age distribution of cinder cones within the Bandas del Sur Formation, southern Tenerife, Canary Islands." Geological Magazine 146, no. 2 (September 16, 2008): 161–72. http://dx.doi.org/10.1017/s001675680800544x.

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AbstractThe Quaternary Bandas del Sur Formation in the south of Tenerife comprises a complex sequence of pyroclastic rocks and lavas. In contrast to the NW- and NE-Rift zone on Tenerife, the S-Rift zone comprises a number of characteristics with respect to the morphological features, eruption cyclicity and the geochemistry of the volcanic deposits. Various flank eruptions of the Las Cañadas volcano associated with basaltic lavas and the formation of cinder cones within the Bandas del Sur are important volcanic units for understanding the explosive volcanic cycles during the Pleistocene on Tene

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Ramm, Mogens. "A stratigraphic study of Late Quaternary sediments on the Vøring-Plateau, eastern Norwegian Sea." Marine Geology 83, no. 1-4 (September 1988): 159–91. http://dx.doi.org/10.1016/0025-3227(88)90057-6.

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