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Dissertations / Theses on the topic 'Neogen'

Author: Grafiati

Published: 4 June 2021

Last updated: 16 June 2025

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1

Rutishauser, Verena. "Das Südtessin im Neogen : zwischen Schuttstrom und Schelfmeer : eine Fazies- und Ablagerungsraumanalyse /." Zürich : [s.n.], 1986. http://e-collection.ethbib.ethz.ch/show?type=diss&nr=7902.

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2

Wiechmann, Marc Filip. "Albanerpetontidae (Lissamphibia) aus dem Mesozoikum der Iberischen Halbinsel und dem Neogen von Süddeutschland." [S.l.] : [s.n.], 2004. http://www.diss.fu-berlin.de/2004/224/index.html.

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3

Hernández, Luján Àngel. "Les tortugues (Testudines) del neogen i quaternari de Catalunya (NE de la Península Ibèrica)." Doctoral thesis, Universitat Autònoma de Barcelona, 2015. http://hdl.handle.net/10803/381065.

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Es revisa el registre neogen i quaternari de les tortugues terrestres i d’aigua dolça (Testudines) de Catalunya, a partir de les restes de la conca del Vallès-Penedès i del pla de Barcelona. A banda d’una revisió bibliogràfica, l’estudi es fonamenta en la descripció i atribució taxonòmica de més de 1.400 restes fòssils (majoritàriament inèdites) procedents de més de 100 localitats. S’emfatitzen aquelles restes que permeten un avenç més significatiu en el coneixement de la sistemàtica, filogènia i/o biostratigrafia de determinats tàxons extints. Respecte a les tortugues terrestres gegants, des

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4

Melnick, Daniel. "Neogene seismotectonics of the south-central Chile margin : subduction-related processes over various temporal and spatial scales." Phd thesis, Potsdam : GeoForschungsZentrum Potsdam, 2007. http://www.gfz-potsdam.de/bib/zbstr.htm.

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5

Renaudie, Johan. "A synthesis of Antarctic Neogene radiolarians." Doctoral thesis, Humboldt-Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät I, 2014. http://dx.doi.org/10.18452/16985.

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Der Südozean ist die Schlüsselregion zur Kenntnis der neogenen Klimaentwicklung. In diesem Zusammenhang ist die Untersuchung von planktonischen Gemeinschaften in Hinblick auf die Umweltentwicklung von großer Bedeutung. In antarktischen neogenen Sedimenten sind Radiolarien reichlich, in großer Diversität und einheitlich gut erhalten. Sie sind nicht nur perfekte Testobjekte für paläobiologischen Studien, sondern auch eine wichtige Quelle für eine verbesserte Biostratigraphie – bisher behinderte nämlich das Fehlen einer verlässlichen Geochronologie detaillierte Studien. Es wurde ein Datensatz al

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6

Forst, Markus H. "Zur Karbonatsedimentologie, Biofazies und sequenzstratigraphischen Architektur eines fossilen Hochenergie-Schelfs aus dem Neogen der Algarve (Miozän, Südportugal)." [S.l. : s.n.], 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=969938292.

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7

Molinu, Anna Rita. "Microbioerosión en substratos esqueléticos del Neógeno y el Cuaternario marinos del Mediterráneo Occidental." Doctoral thesis, Universitat de Barcelona, 2015. http://hdl.handle.net/10803/396601.

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Las perforaciones producidas por microorganismos endolíticos (bacterias, algas, hongos, entre otros) se vienen utilizando en el registro fósil para la interpretación paleoambiental de medios marinos. Las características particulares de estos organismos y de sus trazas permiten identificar zonas fóticas, que a su vez se pueden relacionar con la paleobatimetría relativa. Además, algunas microperforaciones o asociaciones de ellas se utilizan como indicadores paleotermométricos. En la presente memoria se han estudiado mediante técnicas de microscopía electrónica las trazas de microperforación pres

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8

Silveira, Rosemery Rocha da. "Bioestratigrafia e paleoecologia de depósitos neógenos e pleistocenos aflorantes na porção central e ocidental da Bacia do Solimões, Estado do Amazonas, Brasil." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2015. http://hdl.handle.net/10183/132294.

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As 93 amostras palinológicas obtidas deste estudo são oriundas de 12 afloramentos relacionados às formações Solimões e Içá, na região de Coari (5 afloramentos) e Alto Solimões (7 afloramentos), Bacia do Solimões, no estado do Amazonas. Este trabalho apresenta os palinomorfos reconhecidos nestes depósitos (incluindo descrições quando necessárias), com registro fotomicrográfico, relativos a 11 taxons de esporos de fungos, 7 algas, 1 escolecodonte, 1 cisto de dinoflagelado, 31 esporos de pteridófitas, 2 grãos de pólen de gimnospermas e 48 grãos de pólens de angiospermas. Perfis compostos foram co

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9

Warkus, Frank. "Die neogene Hebungsgeschichte der Patagonischen Anden im Kontext der Subduktion eines aktiven Spreizungszentrums." Phd thesis, [S.l. : s.n.], 2002. http://pub.ub.uni-potsdam.de/2002/0024/warkusf.pdf.

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10

Poore, Heather Rachel. "Neogene epeirogeny and the Iceland Plume." Thesis, University of Cambridge, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.612116.

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11

Cross, Lanu. "The Neogene tectonostratigraphic evolution of Java, Indonesia." Thesis, University of London, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.603457.

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This field-based study gives an account of the Neogene structural and stratigraphic development of Java, and the timing and causes of deformation. In this study the stratigraphy and structural domains of Java have been described based on observations made at outcrop. A new stratigraphic scheme for Java is presented calibrated by faties analysis plus forminiferal and nannofossil biostratigraphy. Three separate periods of volcanism have been recognised affecting Java during the Neogene since the extinction of the OJigo-Miocene Arc. Major eruptive episodes occurred between 11.5- lOMa, 6.5-5Ma and

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12

Suggate, Simon Matthew. "Provenance of neogene sandstones of Sabah, northern Borneo." Thesis, University of London, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.542377.

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13

Baggley, Kieron A. "The Late Tortonian - Early Messinian Foraminifera Record of the Abad Member (Turre Formation), Sorbas Basin, Almeria, southeast Spain." Thesis, University of Greenwich, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.389509.

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14

O'Connor, Barry M. "Studies in New Zealand Late Paleogene–Early Neogene Radiolaria." Thesis, University of Auckland, 1996. http://hdl.handle.net/2292/2092.

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Radiolaria from Late Eocene to Early Miocene localities in New Zealand are detailed in a series of studies in an attempt to broaden our knowledge of New Zealand Late Paleogene-Early Neogene Radiolaria, and a new technique for investigating Radiolaria is described. Chapter One introduces the studies and the rationale behind each, details the history of radiolarian work in New Zealand, and provides discussion of several points that surfaced during the studies. The points discussed are: radiolarian literature; plate production; scanning electron micrographs versus transmitted light photomicrograp

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15

Evans, John Rhys. "Late Neogene agglutinated foraminifera from the central Arctic Ocean." Thesis, University College London (University of London), 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.267751.

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16

Rance, Stephanie Jane. "Neogene biogenic silica fluxes in the eastern Equatorial Pacific." Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246232.

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17

Underhill, J. R. "Neogene and Quaternary tectonics and sedimentation in Western Greece." Thesis, Cardiff University, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.376430.

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18

Forde, Emily Jane. "The geochemistry of the neogene Halmahera arc, Eastern Indonesia." Thesis, University College London (University of London), 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.270141.

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The Halmahera arc is a north-south linear intraoceanic arc cutting across the islands of Halmahera and Bacan in NE Indonesia. The arc is the result of the eastward subduction of the Molucca Sea Plate, accommodating the westward movement of the Pacific and Philippine Sea Plates (PSP) against the Eurasian margin. To the south of the Halmahera arc is a major left-lateral strike-slip fault system: the Sorong Fault Zone (SFZ), which separates the northward movement of Australia from the westward movement of the PSP. This plate boundary has been stable throughout the Neogene to the present day, and

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19

Stewart, Duncan Ross McIver. "Evolution of Neogene globorotaliid foraminifera and Miocene climate change." Thesis, University of Bristol, 2003. http://hdl.handle.net/1983/2bd17901-2015-41b6-b43a-acb79c9cdf44.

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20

Vernon, Antoine. "Approche thermochronologique de l'exhumation tardi-Neogene des Alpes Europeennes." Phd thesis, Grenoble 1, 2008. http://www.theses.fr/2008GRE10313.

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Le flux de sédiments en provenance des Alpes montre une importante augmentation 5 Ma). Cette observation, liée à l'exhumation duà la limite Mio-Pliocène ( bassin molassique suisse depuis 5-4 Ma, a conduit à suggérer que les Alpes ont connu une exhumation et un uplift isostatique accélérés à l'échelle de l'orogène depuis cette période. Les objectifs principaux de cette thèse sont de déterminer s'il existe une hausse de l'exhumation alpine après 5 Ma, de préciser son extension spatiale et temporelle, et de passer en revue les différents facteurs potentiels (tectoniques ou climatiques) contrôlan

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21

Sghari, Abdeljalil. "Sedimentation et morphogenese au neogene-quaternaire en tunisie meridionale." Strasbourg 1, 1991. http://www.theses.fr/1991STR10006.

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Les reliefs du sud-ouest tunisien presentent les caracteristiques du relief jurassien avec ses formes d'erosion typiques telles que les combes anticlinales, les monts, les vals, les cluses. . . L'equipement hydrographique des structures de la region montre deux generations hydrographiques : un reseau ante-quaternaire et un reseau quaternaire. Le premier reseau avait ete implique dans la sedimentation neogene du bassin de gafsa. La reconstitution paleomorphologique et l'analyse sedimentologique ont montre que cette region a evolue durant le neogene en bassin sedimentaire quasiment plat qui n'et

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22

Vernon, Antoine. "Approche thermochronologique de l'exhumation tardi-Neogene des Alpes Europeennes." Phd thesis, Université Joseph Fourier (Grenoble), 2008. http://tel.archives-ouvertes.fr/tel-00339424.

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Le flux de sédiments en provenance des Alpes montre une importante augmentation à la limite Mio-Pliocène (⊥5 Ma). Cette observation, liée à l'exhumation du bassin molassique suisse depuis 5-4 Ma, a conduit à suggérer que les Alpes ont connu une exhumation et un uplift isostatique accélérés à l'échelle de l'orogène depuis cette période. Les objectifs principaux de cette thèse sont de déterminer s'il existe une hausse de l'exhumation alpine après 5 Ma, de préciser son extension spatiale et temporelle, et de passer en revue les différents facteurs potentiels (tectoniques ou climatiques) contrôlan

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23

Waters, David William. "The tectonic evolution of Epirus, northwest Greece." Thesis, University of Cambridge, 1994. https://www.repository.cam.ac.uk/handle/1810/251679.

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24

Hooper, P. W. P. "Late Neogene planktonic forminifera and palaeoceanography of the North Atlantic." Thesis, University of East Anglia, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.327884.

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25

Benavente, Escobar Carlos Lenin. "Neogene tectonic and exhumation of the Andes Centrales, Southern Peru." Thesis, Université Grenoble Alpes (ComUE), 2017. http://www.theses.fr/2017GREAU021/document.

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L’histoire et les mécanismes de soulèvement des Andes centrales ont fait l'objet de débats animés depuis les années 1970. Notre étude se concentre sur l’analyse de la déformation Cénozoïque et de l'exhumation des Andes Centrales dans la région du Sud Pérou : à Cuzco, et dans la région de Nazca entre les cordillères Occidentale et Côtière. En effet, plusieurs auteurs soulignent le rôle du raccourcissement tectonique dans l'épaississement de la croûte, dans l’avant-arc Chilien ou à l’Est dans la région Subandine. Dans les modèles de déformation tectonique active issus du GPS, aucun raccourcissem

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26

Curtis, Kathryn Venz. "Oceanic deep-water circulation and climate during the late neogene." [Gainesville, Fla.] : University of Florida, 2004. http://purl.fcla.edu/fcla/etd/UFE0005604.

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27

Baumgartner, Kyrie A. "Neogene Climate Change in Eastern North America: A Quantitative Reconstruction." Digital Commons @ East Tennessee State University, 2014. https://dc.etsu.edu/etd/2348.

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Though much is known of the global paleoclimate during the Neogene, little is understood about eastern North America at that time. During the Neogene the global paleoclimate was transitioning from the warm temperatures and higher levels of precipitation of the Paleogene to the cooler temperatures and lower levels of precipitation during the Pleistocene. Eleven fossil sites from Neogene eastern North America were analyzed using the Coexistence Approach: Pollack Farm, Brandon Lignite, Legler Lignite, Alum Bluff, Bryn Mawr, Big Creek on Sicily Island, Brandywine, Gray Fossil Site, Citronelle, Pea

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28

Balgord, Elizabeth A. "Triassic to Neogene Evolution of the Andean Retroarc: Neuquén Basin, Argentina." Diss., The University of Arizona, 2016. http://hdl.handle.net/10150/595810.

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The Andes Mountains provide an ideal natural laboratory to analyze the relationship between the tectonic evolution of a subduction margin, retroarc shortening, basin morphology, and volcanic activity. Timing of initial shortening and foreland basin development in Argentina is diachronous along strike, with ages varying by 20-30 million years. The Neuquén Basin (32°S-40°S) of southern-central Argentina sits in a retroarc position and provides a geological record of sedimentation in variable tectonic settings from the Late Triassic to the early Cenozoic including: 1.) active extension and deposi

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29

Johnson, Christopher. "Neogene tectonics in South Eastern Spain : constraints from fission track analysis." Thesis, Birkbeck (University of London), 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.326316.

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30

Vernon, Antoine J. "Thermochronological approach to the late Neogene exhumation of the European Alps." Thesis, University of Edinburgh, 2008. http://hdl.handle.net/1842/3181.

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Sediment flux from the Alps shows a sharp increase around the Mio-Pliocene boundary (~5 Ma). This observation, linked to the exhumation of the Swiss Molasse basin since ca. 5-4 Ma has led to the suggestion that the Alps experienced accelerated exhumation and isostatic uplift at the orogen scale since this time. The core objectives of this thesis are to assess whether we can document post 5 Ma exhumation of the Alps and its spatial and temporal development, and to review the different potential (tectonic or climatic) factors controlling this denudation. I have developed a novel technique that u

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31

Bergh, Eugene. "Neogene to quaternary foraminifera from the western margin of southern Africa." Doctoral thesis, Faculty of Science, 2019. http://hdl.handle.net/11427/30436.

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The western margin of southern Africa underwent major palaeoceanographic changes since the initiation of the Benguela Upwelling System during the Neogene. Microfossils in marine sediments provide key proxies in our understanding of how the margin evolved. Fossil shells (tests) of foraminifera (singlecelled protists) from twenty cores from the Namibian shelf (199 to 309 m water depth) and three cores from the western slope (874 to 3631 m water depth) of South Africa were studied to determine the middle Miocene to Quaternary stratigraphy, palaeoenvironment and palaeoceanography of the western ma

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32

SAINT-ANDRE, PIERRE-ANTOINE. "Contribution a l'etude des grands mammiferes du neogene de l'altiplano bolivien." Paris, Muséum national d'histoire naturelle, 1994. http://www.theses.fr/1994MNHN0009.

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Le propos de cette these est de preciser les connaissances que nous avons des grands mammiferes du neogene de l'altiplano. Nous y etudions particulierement les faunes des gisements colloncuriens, huayqueriens et montehermoseens du centre et du nord de l'altiplano bolivien. Nous faisons egalement mention des gisements fossiliferes colloncuriens, chasicoiens et huayqueriens du sud de l'altiplano. La premiere partie traite du cadre geologique de la region etudiee et des correlations stratigraphiques que permettent d'etablir les donnees radiochronologiques obtenues a partir de tufs volcaniques. La

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33

Ochoa-Lozano, Diana. "Neogene Palynology of the Gray Fossil Site, Tennessee, USA: Floristic Implications." Digital Commons @ East Tennessee State University, 2011. https://dc.etsu.edu/etd/2248.

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In order to understand Mio-Pliocene floristic characteristics of the southern Appalachian Mountains, 47 palynological samples from six different testing-pits across the Gray Fossil Site (GFS) were analyzed. The site exhibits a low pollen yield resulting from basic pH levels, drought, and fire events occurring during deposition. The palynofloral assemblage has a low to moderate diversity, and it is largely dominated by Quercus-Carya-Pinus (~90% of the palynoflora). The reported presence of Pterocarya grains supports a Late Neogene age for the lacustrine sediments. Comparison with modern pollen-

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34

Unlugenc, Ulvi Can. "Controls on Cenozoic sedimentation in the Adana Basin, southern Turkey." Thesis, Keele University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.320244.

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35

Arnaoty, Ahmed. "Etude de l'expression de recombinases néogéniques dans le cancer colorectal." Thesis, Tours, 2013. http://www.theses.fr/2013TOUR4012.

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Le phénomène dit de domestication moléculaire qui a été rapporté pour certains transposons à ADN a abouti à la formation de néogènes qui codent des protéines potentiellement impliquées dans la stabilité du génome de part une activité recombinase. L’objectif de ce travail est d’étudier l’expression de 23 recombinases néogéniques d’intérêt dérivées de transpsons à ADN dans une série de cancers colorectaux. Nous avons fabriqué de nouveaux anticorps performants pour l’étude en western blot et en immunofluorescence de l’expression du gène SETMAR qui code pour la protéine Metnase dans des lignées ca

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36

Al-Sabouni, Nadia. "Spatial and temporal size and diversity patterns in neogene-recent planktonic foraminifera." Thesis, Royal Holloway, University of London, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.498251.

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37

Hodgson, David Mark. "Tectono-stratigraphic evolution of a neogene oblique extensional orogenic basin, southeast Spain." Thesis, University College London (University of London), 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.268443.

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38

Preece, Rachel Clare. "The physiological response of equatorial neogene bathyal benthic foraminifera to low oxygen." Thesis, University College London (University of London), 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.314094.

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39

Hinds, David J. "Sedimentology and depositional setting of the Neogene productive series, Aspheron peninsula, Azerbaijan." Thesis, University of Aberdeen, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.400731.

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The largely Pliocene productive Series and its regional equivalents form the major hydrocarbon reservoir unit of the South Caspian Basin. Examination of outcrops and subsurface data from across the Apsheron Peninsula, Azerbaijan, results in the re-interpretation of component depositional environments. Previous studies over-emphasised the role of deltaic processes and lake-level fluctuation in shaping the straitographic architecture of the succession. The repeated juxtaposition of reservoir sandstone and sealing mudstone instead represents the expansion and contraction of terminal fluvial syste

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40

KaÌˆhler, Gisela. "Stratigraphy and sedimentology of the Lefkara Formation, Cyprus : (Palaeogene to early Neogene)." Thesis, University of Southampton, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.241138.

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41

Poole, C. R. "The late Neogene planktonic foraminifera genus Globigerinoidesella : taxonomy, biostratigraphy, evolution and palaeoecology." Thesis, University College London (University of London), 2017. http://discovery.ucl.ac.uk/1557291/.

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Planktonic foraminifera have one of the most complete fossil records of any group, and have proved invaluable in the fields of biostratigraphy, palaeoceanography and evolutionary studies. Gradual morphological change characterises their evolution, meaning that species delimitation for biostratigraphic purposes is typically artificial and arbitrary. Delimited taxa in the fossil record are ‘morphospecies’ rather than biological species. The late Neogene morphospecies Globigerinoidesella fistulosa is of considerable biostratigraphic utility because of its short stratigraphic range (mid-Pliocene t

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42

Boyd, Jamie Lorna. "Global and regional assessment of Neogene climate and palaeoceanography using dinoflagellate cysts." Thesis, University of Leeds, 2016. http://etheses.whiterose.ac.uk/16324/.

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The Neogene Period (23.03–2.59 Ma) has been referred to as ‘the making of the Modern world’, which eventually, via a relatively consistent cooling trend, culminated in the present day climate conditions on Earth. Researching the Neogene provides important information for understanding how modern patterns of atmospheric and oceanic circulation developed, and how sensitive they are to environmental change. Climate and environmental parameter proxies are used to investigate past changes, and dinoflagellate cysts have great potential as their distribution can be limited by temperature, salinity, n

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43

Rowan, Christopher James. "Neogene paleomagnetism and geodynamics of the Hikurangi margin, East Coast, New Zealand." Thesis, University of Southampton, 2006. https://eprints.soton.ac.uk/41330/.

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Vertical-axis rotations are an important component of Neogene deformation in the New Zealand plate boundary region, and potentially offer fundamental insights into the rheology of continental crust. Extensive paleomagnetic sampling along the Hikurangi margin, on the East Coast of the North Island, has provided new insights into the patterns, rates and timings of tectonic rotation, and also an improved understanding of the magnetic signature of New Zealand Cenozoic mudstones. Rigorous field tests reveal numerous late remagnetizations, which haveoften formed several million years after depositio

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44

Rees-Owen, Rhian Laura. "Antarctic climate and vegetation during the Neogene : a geochemical and modelling approach." Thesis, University of Leeds, 2016. http://etheses.whiterose.ac.uk/15445/.

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During the mid- to late Neogene (20 - 2.5 million years ago), episodic retreat of the Antarctic Ice Sheet (AIS) coincided with periods of higher-than-present atmospheric CO2, indicating ice sheet sensitivity to climatic conditions similar to those projected for the coming decades. Understanding Antarctic climate and vegetation during such a period of AIS retreat is crucial for our fundamental understanding of high latitude environments in warmer-than-present climate scenarios. This thesis presents a detailed geochemical study of sediments and plant fossils from the terrestrial Sirius Group of

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45

Madden, Robert Henry Christopher. "Modern and neogene analogues for productive subsurface carbonate systems in SE Asia." Thesis, Curtin University, 2013. http://hdl.handle.net/20.500.11937/2072.

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This combined sedimentological, diagenetic and remote sensing study of SE Asian Cenozoic carbonate systems has implications for the understanding of how depositional and diagenetic conditions unique to the equatorial tropics influence regional hydrocarbon reservoir development. Most modern analogues used to help evaluate carbonate development and their subsurface reservoir potential are from sub-tropical to arid regions. However, within carbonate build-ups some of the world’s most prolific hydrocarbon reserves are in Neogene subsurface deposits from SE Asia where the models generated in other

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46

Titchener, Frederick Robert. "Plant-arthropod interactions in the late Tertiary." Thesis, Royal Holloway, University of London, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.482120.

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47

Patterson, Molly O’Rourke. "FORAMINIFERA FAUNA RECOVERED FROM ANDRILL’S (ANtarctica geological DRILLing program) SOUTHERN MCMURDO SOUND (SMS) PROJECT." OpenSIUC, 2010. https://opensiuc.lib.siu.edu/theses/411.

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During the Austral Spring of 2007-2008 the ANtarctic geological DRILLing program (ANDRILL) recovered a 1,138 meter long sediment core AND-2A from the western side of the Victoria Land Basin for the Southern McMurdo Sound Project. The main goal of the project is to help establish a Neogene (~24 to 1.6 Mya) ice volume and climate record of Antarctica. This study focuses on the foraminifera record of AND-2A for paleoenvironmental and biostratigraphic purposes.AND-2A is unique in that it contains a Middle Miocene record (~17 to ~11 Mya) that includes the Middle Miocene transition of warm climatic

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48

Stevens, Anthony. "NEOGENE PALEO-ENVIRONMENTAL ANALYSIS OF QUEBRADA LA HIGUERA SECTION, BAHIA INLGESA, NORTHERN CHILE." OpenSIUC, 2010. https://opensiuc.lib.siu.edu/theses/283.

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Marine sediment samples were collected from Quebrada la Higuera, Chile to provide a record of planktonic and benthic foraminifera as a means of reconstructing the paleo-bathymetry and paleo-environment of the Quebrada la Higuera basin. The research area is located in northern Chile, south of Caldera in Quebrada la Higuera (S 27° 16.443, W 70° 54.887). The Quebrada la Higuera basin rests unconformably atop Mesozoic gabbroic basement, which is locally exposed, representing fault-bounded horsts and grabens. At the base of the section, diatomaceous sediment within the sequence suggests interval

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Johnson, Katherine. "Deep-water foraminifera of the Kerguelen Plateau responses to climate in the late Neogene /." Columbus, Ohio : Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1211895313.

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Mannan, A. (Abdul). "Stratigraphic evolution and geochemistry of the Neogene Surma Group, Surma Basin, Sylhet, Bangladesh." Doctoral thesis, University of Oulu, 2002. http://urn.fi/urn:isbn:9514267117.

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Abstract The Surma basin is a part of the Bengal Basin situated in northeastern Bangladesh. The presence of eight gas fields and one oil field makes this an area that is interesting both economically and geologically. In spite of detailed geological and geophysical investigations, information available on palynostratigraphy and geochemistry for the area is scanty. The aim of the present work was to investigate the palynological assemblages, mineralogy and geochemistry of the Surma Group (SG) sequences in Surma Basin, Bangladesh. Core samples (n = 188) were gathered from the wells following: P

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