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3 edition of Clay mineral stratigraphy of Miocene to Recent marine sediments in the central Mediterranean found in the catalog.

Clay mineral stratigraphy of Miocene to Recent marine sediments in the central Mediterranean

Clay mineral stratigraphy of Miocene to Recent marine sediments in the central Mediterranean

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Published by Instituut voor Aardwetenschappen Rijksuniversiteit in Utrecht .
Written in English

    Subjects:
  • Clay minerals - Mediterranean

  • Edition Notes

    11

    The Physical Object
    Pagination244 p.
    Number of Pages244
    ID Numbers
    Open LibraryOL21986144M
    ISBN 109071577295

      The Alaşehir (Gediz) Graben exemplifies clastic sedimentation in a long-lived continental half-graben in a semi-arid setting, developed within relativ


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Clay mineral stratigraphy of Miocene to Recent marine sediments in the central Mediterranean Download PDF EPUB FB2

Abstract. X-ray diffraction analyses were made of the smaller than 2 fraction from\ud about samples of the central Mediterranean Miocene to Recent and the\ud southeastern North-Atlantic Miocene in order to reconstruct climatic changes.\ud Relative quantities of the clay minerals chlorite, illite, pyrophyllite, smectite,\ud kaolinite and palygorskite and the accessory minerals quartz Clay mineral stratigraphy of Miocene to recent marine sediments in the central Mediterranean.

The influence of a deteriorating climate is envisaged for the Middle Miocene and Pleistocene. Clay compositional changes in the Middle Miocene of the two study areas also reflect rejuvenation of reliefs and possibly changing wind and current The Longzhong Basin is situated in the transition zone between the Chinese Loess Plateau and Northeastern Tibetan Plateau, and is surrounded by the Liupan Mountains, West Qinling Mountains and Qilian Mountains (Fig.

1A).It is composed of several sub-basins: from west to east, these are the Xining Basin, Lanzhou Basin, Linxia Basin and Longxi-Jingning Basin, each containing thick Cenozoic We have studied damage zones of two active faults, Baza and Padul faults in Guadix-Baza and Granada basins, respectively, in South Spain.

Mineral and microstructural characterization by X-ray diffraction and field emission electron microscopy studies have been combined with structural fieldwork and in situ measurements of rock properties (permeability and Young’s modulus) to find out the Stratigraphy of the Oligocene-Miocene boundary sediments in the Nezhinsky brown coal field (Primorye) and the problem of the Paleogene-Neogene boundary in the region intreprated as deep marine The isolation and separate evaluation of the impact of these various factors on clay-mineral distribution in marine sediments, as attempted in these works, is the only way in which the paleoclimatic interpretation of clay minerals in marine sediments can be expected to yield significant :// 4.

Clay mineral origin in the central Mediterranean. In all the sections, two groups of minerals showing opposite cyclic variations can be distinguished. The first is mainly characterized by kaolinite and palygorskite whose abundance variations display the same pattern as that of carbonate :// Seismic stratigraphy of the Miocene-Pleistocene sedimentary basins of the Northern Tyrrhenian Sea and Western Tuscany (Italy) December Basin Research 11(4) Middle to late Miocene sequence stratigraphy of the Transylvanian Basin (Romania) Article in Clay mineral stratigraphy of Miocene to Recent marine sediments in the central Mediterranean book (1) December with Reads How we measure 'reads' The sediments in the eastern Laptev Sea and the East Siberian Sea are characterized by increased contents of illite [Wahsner et al., ], and are considered as a source for the fine fraction in Subunits 1/3 and 1/4.

The changes in the clay and heavy mineral assemblages do not occur exactly in :// Clay mineral stratigraphy of Miocene to Recent marine sediments in the central ().

Contribution • l'6tude des foraminif•res de la M6diterra6e: Relations entre le microfaune et le s6diment' Biocoenoses actuelles, thanatocoenoses plioc•nes et quaternaires, Mid-Miocene climatic optimum: Clay mineral evidence from the red clay succession, Longzhong Basin, Northern China October Palaeogeography Palaeoclimatology Palaeoecology Sedimentary facies, mineralogy, and geochemistry of the sulphate-bearing Miocene Dam Formation in Qatar Article in Sedimentary Geology (1) January with Reads How we measure Miocene extensional sedimentary basins are being increasingly recognized in Central Mediterranean.

However the paleogeographic reconstruction of the Paleo-Tyrrhenian during this time span results a difficult task because the subsequent Pliocene-Quaternary backarc opening moved away these older sedimentary :// Palygorskite is frequently present in the Cretaceous sediments of the Atlantic Ocean.

Here, we will examine palygorskite clay distribution in Albian and Aptian sediments in three DSDP drill sites (, and ) that are situated on an approximately East–West transect through the Central Atlantic Ocean ().Download: Download full-size image Clay mineral variations in Holocene terrestrial sediments from the Indus Basin - Volume 77 Issue 3 - Anwar Alizai, Stephen Hillier, Peter D.

Clift, Liviu Giosan,   Diagenetic clay mineral distribution is constrained along sequence and parasequence boundaries, and within parasequences, parasequence sets and systems tracts. 23 Paper V – In this paper, we discuss the sequence stratigraphic distribution and origin  › 百度文库 › 互联网.

Clay mineral and quartz contents of sediments from two western North Pacific DSDP sites record a history of paleoclimatic and paleoceanographic conditions of the last 65 million years. DSDP Site has recorded an eolian signal of terrigenous material that was transported from ://   Marine & Petroleum Geology,Cao L, Shao L, Qiao P, et al.

Geochemical evolution of Oligocene–Middle Miocene sediments in the deep-water area of the Pearl River Mouth Basin, northern South China Sea[J]. Marine & Petroleum Recent deformation caused partial inversion of older normal faults and is concentrated along major fault zones like the Alboran ridge-Xauen bank alignment in the central Alboran Sea (e.g., Bourgois et al., ; Chalouan et al., ) or the Yusuf fault zone in the transition to the Algerian Basin (e.g., Álvarez-Marrñn, ; Domzig et al Clay mineral distribution in surface sediments of the northeastern South China Sea and surrounding fluvial drainage basins: Source and transport.

Marine Geology, Colin, C.*, Siani, G., Sicre, M.-A., Liu, Z., Impact of the East Asian monsoon rainfall changes on the erosion of the Mekong River basin over the p yr Abstract.

The highly complex morphology of the continental slope of central Israel is the expression of deep-seated rotational block slumping. The overburden of – km thick Pliocene-Quaternary sediments that accumulated over m thick evaporites deposited under the deeper portion of the present-day continental slope and in Late Miocene erosion channels, caused the evaporites to flow   Deep-water Sedimentary Systems: Thematic Set, Marine and Petroleum Geology, Vol No.

ten Veen, Johan H. and Postma, George,"Astronomically forced variations in gamma-ray intensity; late Miocene hemipelagic successions in the eastern Mediterranean basin as a test case", Geology; January v. 24; no. 1; p. ?pageid= Abstract. ODP drilling in the Norwegian Sea (Leg ) and Baffin Bay (LegSite ) provided the first continuous cores for study of Neogene to recent paleoclimatic changes in the circum-Arctic basins of the North :// 2.

Geological Setting, Section, and Lithology [6] The sediments of the Globigerina Limestone and Blue Clay Formation on Malta and Gozo were deposited in the Maltese Graben System, a series of Miocene‐Quaternary extensional basins that developed on the African foreland of the Sicilian Apennine‐Maghrebian fold and thrust belt [De Visser, ; Dart et al., ].

Abstract. In central eastern Anatolia which is located between Eurasia and Africa, the study of basin developments between late Eocene and early Miocene is of great importance for understanding the process of the closure of the Neo-Tethys Ocean and the   @article{osti_, title = {Stratigraphy of the Sarkisla area, Sivas basin, eastern central Anatolia}, author = {Bilgic, T and Sumengen, M and Terlemez, I and Unay, E and Gurbuz, M and Erkan, E}, abstractNote = {The stratigraphy of the Sarkisla area, southeastern Central Anatolian Massif, is characterized by a succession of rock units ranging from late Paleocene to Pliocene in ://   Astronomical forcing of sedimentary cycles in the middle to late Miocene continental Calatayud Basin (NE Spain) H.

Abdul Aziza;*, F. Hilgena, W. Krijgsmanb, E. Sanzc, J.P. Calvod a Department of Geology, Faculty of Earth Sciences, Utrecht University, Budapestlaan 4, CD Utrecht, The Netherlands b Paleomagnetic Laboratory ‘Fort Hoofddijk’, Utrecht University, Budapestl Click on the book chapter title to read ://   @article{osti_, title = {Maturation history of Neogene-Quaternary sediments, Nile delta basin, Egypt}, author = {El-Ella, Ramadan Abu}, abstractNote = {The present Nile delta area covers approximat km{sup 2}.

Fields in this area provide two-thirds of the gas production in Egypt. Geological knowledge of the Nile delta is still limited because of insufficient subsurface :// Tomadin L., - Provenance and dispersal of clay minerals in recent sediments of the Central Mediterranean Sea.

In: Sedimentary Basins of Mediterranean Margins (F. Wezel Ed.), CNR Italian Project of Oceanography, Tecnoprint, Bologna, – Google Scholar   Publications of Mark Dekkers: Asian monsoon modulation of non-steady state diagenesis in hemipelagic marine sediments offshore of Japan.

Geochem. ,I., Palcu, D.V., Dekkers, M.J. and Krijgsman, W. () A greigite-based magnetostratigraphic time frame for the Late Miocene to Recent DSDP Leg 42B cores from the Black Sea. ~forth/people/Mark/   CiteScore: ℹ CiteScore: CiteScore measures the average citations received per document published in this title.

CiteScore values are based on citation counts in a given year (e.g. ) to documents published in three previous calendar years (e.g.

– 14), divided by the number of documents in these three previous years (e.g. – 14). The magnetic mineral assemblages of Miocene clay sediments in upper unit II at IODP Holes MA and MA are dominated by greigite.

Although we find some evidence for a primary magnetic phase (A2), the paleomagnetic signal is most likely a record of one or several remagnetization :// The Middle Miocene (Badenian) evaporites of the northern Carpathian Foredeep were deposited in a salina-type basin. Calcium sulphate sediments were deposited mainly on the broad northern margins of the basin, on vast evaporite shoals (mainly as fine-grained microbialite gypsum) and in large shallow saline pans (as coarse-crystalline selenites).

sections of these primary deposits, exposed (b) Middle Miocene: Latakia and Margat Ridges are active, with mid‐Miocene sediments onlapping on the inclined early Miocene sediments.

Normal faults are initiating in the Levant Basin. (c) late Miocene: continuous activity of the Latakia, Margat, and Larnaca Ridges Evidence for Late Miocene Mediterranean overflow from bottom current deposits within the Rifian Corridor (Morocco) Dr.

Javier Hernández-Molina: Morphology and Stratigraphy of the Central California Shelf - Results from the California Seafloor and Coastal Mapping Program: Dr. Samuel   Symposium on Recent and Fossil Marine Diatom, Nova Hedwigia,39, – Google Scholar [15] Burckle L., Early Miocene to Pliocene diatom datum levels for the equatorial Pacific, Proceedings of the Second Working Group Meeting, Biostratigrafic Datum Planes of the Pacific Neogene, IGGP ProjectBadung, Indonesia, Geol.

Res. and :// Kennett, J.P. Paleo-oceanographic Aspects of the Foraminiferal Zonation in the Upper Miocene-Lower Pliocene of New Zealand. Committee Mediterranean Neogene Stratigraphy Proc. IV Session. Giornale di Geologia Annali Del Museo Geologico de Bologna Thus, Miocene sediments in the central and southeastern Alboran Sea are probably younger and thinner than those in the western and northern parts of the basin.

Onshore‐offshore correlations indicate that the Boudinar and Melilla basins are the emergent parts of the SAB (Achalhi et.

The stratigraphic and structural evolution of the Pattani basin, the most prolific petroleum basin in Thailand, reflects the extensional tectonics of continental southeast Asia. East-west extension, a product of the northward collision of India with Eurasia since the early Tertiary resulted in the Alternating Southern and Northern Hemisphere climate response to astronomical forcing during the past 35 m.y.

A shift in heavy and clay mineral provenance indicates a middle Miocene onset of a perennial sea ice cover in the Arctic Ocean: Evidence for ice-free summers in the late Miocene central   ROBERT, C., L. DIESTER-HAASS and J. PATUREL ().

"Clay mineral assemblages, siliciclastic input and paleoproductivity at ODP Site off Southwest Africa: A late Miocene-early Pliocene history of Orange river discharges and Benguela current activity, and their relation to global sea level change." Marine Geology (4):