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Bibliografie tematiche / Jurassic stratigraphy

Letteratura scientifica selezionata sul tema "Jurassic stratigraphy"

Autore: Grafiati

Pubblicato: 8 giugno 2024

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Articoli di riviste sul tema "Jurassic stratigraphy":

1

Zeiss, Arnold. "The Upper Jurassic of Europe: its subdivision and correlation". Geological Survey of Denmark and Greenland (GEUS) Bulletin 1 (28 ottobre 2003): 75–114. http://dx.doi.org/10.34194/geusb.v1.4649.

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In the last 40 years, the stratigraphy of the Upper Jurassic of Europe has received much attention and considerable revision; much of the impetus behind this endeavour has stemmed from the work of the International Subcommission on Jurassic Stratigraphy. The Upper Jurassic Series consists of three stages, the Oxfordian, Kimmeridgian and Tithonian which are further subdivided into substages, zones and subzones, primarily on the basis of ammonites. Regional variations between the Mediterranean, Submediterranean and Subboreal provinces are discussed and correlation possibilities indicated. The durations of the Oxfordian, Kimmeridgian and Tithonian Stages are reported to have been 5.3, 3.4 and 6.5 Ma, respectively. This review of the present status of Upper Jurassic stratigraphy aids identification of a number of problems of subdivision and definition of Upper Jurassic stages; in particular these include correlation of the base of the Kimmeridgian and the top of the Tithonian between Submediterranean and Subboreal Europe. Although still primarily based on ammonite stratigraphy, subdivision of the Upper Jurassic is increasingly being refined by the incorporation of other fossil groups; these include both megafossils, such as aptychi, belemnites, bivalves, gastropods, brachiopods, echinoderms, corals, sponges and vertebrates, and microfossils such as foraminifera, radiolaria, ciliata, ostracodes, dinoflagellates, calcareous nannofossils, charophyaceae, dasycladaceae, spores and pollen. Important future developments will depend on the detailed integration of these disparate biostratigraphic data and their precise combination with the abundant new data from sequence stratigraphy, utilising the high degree of stratigraphic resolution offered by certain groups of fossils. This article also contains some notes on the recent results of magnetostratigraphy and sequence chronostratigraphy.

2

Matthews, Robley K., e Cliff Frohlich. "Maximum flooding surfaces and sequence boundaries: comparisons between observations and orbital forcing in the Cretaceous and Jurassic (65-190 Ma)". GeoArabia 7, n. 3 (1 luglio 2002): 503–38. http://dx.doi.org/10.2113/geoarabia0703503.

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ABSTRACT We have undertaken a simplified calculation of orbital forcing back through the Cretaceous to the Late to Middle Jurassic from 65 to 190 Ma. So long as the Earth has a continental ice volume, orbital forcing will impose a 400-ky periodicity upon glacioeustasy and thereby on fourth-order sequence stratigraphy cycles. Similarly, third-order cycles were defined by orbital forcing of 2.4 ± 0.4 my (predominately 2.0- and 2.8-my cycles). These concepts greatly simplified the task of unraveling sequence stratigraphy. Our sea-level calculations are comparable with stratigraphic observations and the results are consistent with a persistent continental ice volume throughout the Late to Middle Jurassic and Cretaceous. In general, they compare well with the Arabian Plate Maximum Flooding Surfaces and the Cretaceous and Jurassic stage boundaries, within the limits of the recognized stratigraphic time scales. We used simple Parametric Forward Models (PFMs) for modeling changes in sea level, subsidence, and sedimentation and noted that PFMs can be applied to other tasks. The results will provide for rapid, cost-effective forward modeling on tasks such as reservoir characterization and flow simulation.

3

Ivanova, Daria. "Cadosinidae Wanner, 1940 and Stomiosphaeridae Wanner, 1940 (Incertae sedis) from the Upper Jurassic of the Central Forebalkan, Bulgaria". Geologica Balcanica 24, n. 6 (30 dicembre 1994): 85–102. http://dx.doi.org/10.52321/geolbalc.24.6.85.

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Representatives of the Incertae sedis group have been studied from Upper Jurassic sequences in the Central Forebalkan. Their taxonomy and stratigraphic range are objects of this paper. Within the stratigraphic sequence of Lower Oxfordian to Upper Tithonian the limestones of the Javorec, Ginci, Gložene and Neškovci Formations are investigated. This paper is a first attempt for careful study of this important for the Upper Jurassic stratigraphy group. 16 species, belonging to 7 genera have been described. They are related to two families: Cadosinidae Wanner, 1940 and Stomiospaeridae Wanner, 1940.

4

Piasecki, Stefan, John H. Callomon e Lars Stemmerik. "Jurassic dinoflagellate cyst stratigraphy of Store Koldewey, North-East Greenland". Geological Survey of Denmark and Greenland (GEUS) Bulletin 5 (1 novembre 2004): 99–112. http://dx.doi.org/10.34194/geusb.v5.4810.

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The Jurassic of Store Koldewey comprises a Middle Jurassic succession towards the south and an Upper Jurassic succession towards the north. Both successions onlap crystalline basement and coarse sediments dominate. Three main lithostratigraphical units are recognised: the Pelion Formation, including the Spath Plateau Member, the Payer Dal Formation and the Bernbjerg Formation. Rich marine macrofaunas include Boreal ammonites and the successions are dated as Late Bathonian – Early Callovian and Late Oxfordian – Early Kimmeridgian on the basis of new collections combined with material in earlier collections. Fine-grained horizons and units have been analysed for dinoflagellate cysts and the stratigraphy of the diverse and well-preserved flora has been integrated with the Boreal ammonite stratigraphy. The dinoflagellate floras correlate with contemporaneous floras from Milne Land, Jameson Land and Hold with Hope farther to the south in East Greenland, and with Peary Land in North Greenland and Svalbard towards the north. The Middle Jurassic flora shows local variations in East Greenland whereas the Upper Jurassic flora gradually changes northwards in East Greenland. A Boreal flora occurs in Peary Land and Svalbard. The characteristic and stratigraphically important species Perisseiasphaeridium pannosum and Oligosphaeridium patulum have their northernmost occurrence on Store Koldewey, whereas Taeniophora iunctispina and Adnatosphaeridium sp. extend as far north as Peary Land. Assemblages of dinoflagellate cysts are used to characterise significant regional flooding events and extensive sequence stratigraphic units.

5

Stemmerik, Lars. "The Jurassic of North-East Greenland". Geological Survey of Denmark and Greenland (GEUS) Bulletin 5 (1 novembre 2004): 1–7. http://dx.doi.org/10.34194/geusb.v5.4799.

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The Jurassic rift succession of East Greenland has been intensely studied over the last 25 years, particularly within the main outcrop areas of Jameson Land and Wollaston Forland. The more isolated and poorly known outcrops on Traill Ø, Hold with Hope, Hochstetter Forland and Store Koldewey were investigated in the late 1980s and mid-1990s in order to develop a better regional understanding of the Jurassic in eastern Greenland.This collection of seven papers focuses on stratigraphic and depositional aspects of the Jurassic at these localities. Comprehensive descriptions of the Jurassic on Hold with Hope and south-eastern Traill Ø are accompanied by papers covering fluvial deposits and new ammonite collections from the Middle Jurassic of Traill Ø. The bulletin is concluded by studies of the dinoflagellate cyst stratigraphy of the Middle and Upper Jurassic of Hold with Hope, Hochstetter Forland and Store Koldewey.

6

Rahman, Mat Niza Bin Abdul. "Jurassic-Cretaceous Stratigraphy of Malaysia". Open Journal of Geology 09, n. 10 (2019): 668–70. http://dx.doi.org/10.4236/ojg.2019.910070.

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7

Ager, Derek V. "Brachiopod stratigraphy in the Jurassic". Geobios 27 (dicembre 1994): 57–68. http://dx.doi.org/10.1016/s0016-6995(94)80125-8.

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8

Michalík, Jozef, Daniela Reháková, Eva Halásová e Otília Lintnerová. "The Brodno section — a potential regional stratotype of the Jurassic/Cretaceous boundary (Western Carpathians)". Geologica Carpathica 60, n. 3 (1 giugno 2009): 213–32. http://dx.doi.org/10.2478/v10096-009-0015-2.

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The Brodno section — a potential regional stratotype of the Jurassic/Cretaceous boundary (Western Carpathians) Compared to coeval successions from the Carpathians, the continuous Jurassic-Cretaceous (J/K) pelagic limestone succession of the Brodno section offers the best possibility to document the J/K passage in a wide area. This section comprises a complete calpionellid, and nannofossil stratigraphic record, that supports the older paleomagnetic data. Moreover, the sequence stratigraphy and stable isotope (δ18O, δ13C) data gave important results, too, enabling comparison with known key sections from the Mediterranean Tethys area.

9

Morton, Nicol. "The International Subcommission on Jurassic Stratigraphy". Proceedings of the Geologists' Association 119, n. 1 (gennaio 2008): 97–103. http://dx.doi.org/10.1016/s0016-7878(08)80261-1.

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Al-Husseini, Moujahed, e Robley K. Matthews. "STRATIGRAPHIC NOTE: Jurassic-Cretaceous Arabian orbital stratigraphy: The AROS-JK Chart". GeoArabia 13, n. 1 (1 gennaio 2008): 89–94. http://dx.doi.org/10.2113/geoarabia130189.

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Tesi sul tema "Jurassic stratigraphy":

1

Parkinson, D. Neil. "The sequence stratigraphy of the Lower Jurassic of Western Europe". Thesis, University of Oxford, 1994. http://ora.ox.ac.uk/objects/uuid:cddbc521-f687-41dd-a9ad-f70621012555.

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The Lower Jurassic stratigraphy of seven contrasting areas in western Europe is compared in order to seek evidence for a pan-Western European stratigraphic forcing mechanism. Sequencestratigraphic models are discussed and emphasis is placed upon the differing response of sedimentary systems in "accommodation space-dominated" and "supply-dominated" settings. Spectral gamma-ray data from clastic successions in the Wessex and Cleveland basins (England) are used to elucidate vertical trends. A proximal-distal model for control of Th/K ratios is advanced. Stage-frequency regressive-transgressive cycles in the two areas are shown to be closely correlative. Sedimentolgical logs and spectral gamma-ray data are presented for the carbonate ramp into turbidite sequence of Peniche (Portugal) and for a new exposure of the Pliensbachian-Toarcian in southern Germany. Systematic variation in clay mineralogy across Europe is suggested. Cycles in the Lower Jurassic of the North Viking Graben (Norwegian North Sea) are examined using wireline log correlation and the stratigraphic evolution of the Tethyan Rift in the Western and Southern Alps is reviewed. X-ray diffraction studies of the Pliensbachian-Toarcian interval in the Southern Alps are presented in order to elucidate sediment supply to the pelagic realm. The cycles observed in the English sections appear to be manifest widely across western Europe in a variety of tectonic and sedimentary settings. Sharp basinward facies shifts (candidate sequence boundaries) do not appear to be synchronous between basins. ⁸⁷SR/⁸⁶SR analysis of belemnites from the Portuguese and German sections confirms the regional applicability of the results of Jones (1992) and the utility of this technique in long range correlation. Carbon and oxygen analysis of the same material supplements the data of other workers and a direct relationship is suggested between relative sea level and organic carbon burial in the Early Jurassic.

2

Ahmadi, Ziad M. "Sequence stratigraphy using wireline logs from Upper Jurassic of England". Thesis, Durham University, 1997. http://etheses.dur.ac.uk/1644/.

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3

Al-Mojel, Abdullah. "Sedimentology and sequence stratigraphy of the Jurassic, Jabal Tuwaiq, Central Saudi Arabia". Thesis, Bordeaux 3, 2017. http://www.theses.fr/2017BOR30037/document.

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Cette étude porte sur l’analyse des séries jurassiques du Shaqra Group (Toarcian to Kimmeridgian) qui affleurent de manière continue en Arabie centrale le long d’un transect de plus de 1000 km de long. Ces séries se sont accumulées sur une vaste plate-forme épicontinentale peu profonde, en contexte tropical. Ces affleurements permettent ainsi d’observer la partie occidentale des séries renfermant des systèmes pétroliers prolifiques exploités en subsurface en Arabie Saoudite. L’analyse sédimentologique de nombreuses coupes et la réalisation de corrélations stratigraphiques de haute résolution sur un transect de 600 km au sud de Riyad, complété par des corrélations avec les données de forage plus à l’est (entre Riyadh et le Rimthan Arch), permettent de distinguer une organisation séquentielle à différents ordres de fréquence et de reconstituer l’évolution de la plate-forme au sein de ces séquences. La plate-forme jurassique évolue d’une plate-forme horizontale caractérisée par des systèmes mixtes à la transition continental-marin du Toarcien au Callovien moyen (formations Marrat et Dhruma) vers un système de type rampe - bassin intrashelf du Callovien au Kimméridgien inférieur (formations Tuwaiq et Hanifa) pour finir par une plate-forme aggradante carbonatée et silico-clastique (Fm. Jubaila) puis carbonatée et évaporitique en contexte aride (Fm. Arab) au Kimméridgien. Les cycles tectono-stratigraphiques de 2ème ordre du Jurassique inférieur et moyen sont limités à la base et au sommet par des discontinuités régionales. Ils occupent un dépôt-centre stationnaire et décrivent un onlap côtier de grande ampleur avec un maximum transgressif au Callovien moyen (Upper Tuwaiq Mb.). Durant le Jurassique supérieur, les dépôts de rampe carbonatée de la Formation Hanifa passent progressivement vers l’ouest à des dépôts plus profonds de bassin intrashelf relativement riches en matière organique (Khurais - Rimthan Arch). La séquence Jubaila – Arab-D montre des variations d’épaisseur qui indiquent une déformation de grande longueur d’onde de la plate-forme arabe à cette période. Les faciès récifaux du membre Arab D sont interprétés comme représentant le maximum d’inondation de ce cycle qui se termine par le développement de systèmes carbonatés – évaporitiques à la fin du Jurassique
They serve as westernmost reference for adjacent prolific reservoirs and source-rock bearing intrashelf basins. Several hierarchical sequences (second to fourth order) have been recognized in outcrops sections (600 km long south of Riyadh) and correlated with gamma-ray logs of subsurface wells (550 km long from Riyadh to Rimthan Arch). The Jurassic platform evolved from very-flat continental-to-nearshore mixed carbonate-siliciclastic platform (Marrat-Dhruma; Toarcian to Middle Callovian) to differentiated ramp with deep intrashelf basins (Tuwaiq-Hanifa; Callovian to Early Kimmeridgian) to a lowstand followed by flat aggraded platform (Jubaila-Arab-D; Kimmeridgian). Tectonic related siliciclastic influx took place in arid condition during the Kimmeridgian (Jubaila Fm.). The Jurassic platform ends with the mixed carbonate-evaporite systems of the Arab Fm. A first second-order tectono-eustatic cycle (Marrat to Tuwaiq) is bounded at the base and top by regional unconformities. It has a stationary depocenter, and show long-term coastal onlap and marine transgression that reached its maximum extent during the upper Tuwaiq (Middle Callovian). The Hanifa Fm. consists of four 3rd-order sequences aggraded flat-toped platform (outcrops to Khurais) marked at the base by argillaceous limestone and top by pure high-energy carbonates with localized reef buildups. The Jubaila Arab-D is two 3rd-order sequences begin with low-stand deposits followed by long-term transgression. These formed flat successions with lateral thickness variations controlled by differential subsidence increased in the Arabian Basin. The transgression is marked by storm-influenced inner-platform with sandstone quartz, grainstones and restricted lime-mudstone. The Maximum marine transgression is placed in the Arab-D with reef buildups in the westernmost inner-platform. During highstand, the reefs are gently prograding out into Rimthan Arch leaving behind restricted lagoon and sabkhah/salina anhydrite

4

Ceglar, Nathan. "Late Jurassic to Early Cretaceous sequence stratigraphy, Northern Bonaparte Basin, Timor Sea /". Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbc389.pdf.

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5

Groecke, Darren Richard. "Isotope stratigraphy and ocean-atmosphere interactions in the Jurassic and Early Cretaceous". Thesis, University of Oxford, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.393117.

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6

Maxwell, Gregor. "The sedimentology and sequence stratigraphy of the Middle Jurassic Beryl Formation, Quad 9, U.K.C.S". Thesis, University of Aberdeen, 1999. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=236949.

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Quad 9 of the U.K.C.S., North Sea is located 215 miles NE of Aberdeen. It contains four producing fields with over 400 mmbbls of oil and NGL's and 5.1 TCF of gas initially in place. The major reservoir unit is the Middle Jurassic (Bajocian to Bathonian) Beryl Formation, a marginal to shallow marine deposit which varies in thickness from 150' to 1100' across the studied area. It was deposited within the Beryl Embayment, a transfer zone between two actively extending basin bounding faults of the South Viking Graben, prior to the onset of the major rifting phase during the Callovian to Ryazanian. The objectives of the thesis were to provide a revised sedimentological model for the area accounting for the contrasting sedimentary styles present within the Beryl Formation and to unify the different correlation schemes used by the different operating companies in the area. It was based on well data from 58 cored and a further 79 uncored sections spreading nine licence blocks within Quad 9. Reservoir engineering, biostratigraphic and structural data has also been used for a fully integrated study. Initial core logging identified 32 facies and 10 trace fossil assemblages which were subsequently integrated into 14 facies associations. These were then extrapolated further into the uncored sections by wireline facies associations. Correlation was initially driven by comparison of cored sections but finalised by an integration of the reservoir engineering and biostratigraphic data. Outcrop work on the Middle Jurassic of Skye and Companian of eastern Utah provided an analogue study to accompany the downhole data. Quad 9 can be split up into three main areas distinguished by different stratigraphic histories, the southern area consisting of the Buckland and Sorby Fields, the central area consisting of the Beryl, Nevis, Ness and Linnhe Fields and a northern area consisting the Bruce and Keith Fields.

7

Zerezghi, Simret Ghirmay. "Sedimentology and Stratigraphy of the Lower Jurassic Portland Formation, Newark Supergroup, Hartford Basin". Ohio University / OhioLINK, 2007. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1181233653.

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8

Cole, David Charles. "Sequence palynology of the lower jurassic (Sinemurian - Toarcian) strata of N W Europe". Thesis, University of Southampton, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.342883.

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9

Molgat, Marianne Patricia. "Sedimentology, stratigraphy, and shallow burial alteration of the Upper Jurassic Swift Formation, southeastern Alberta". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0016/MQ57146.pdf.

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10

James, D. P. "Stratigraphy, sedimentology and diagenesis of Upper Jurassic and Lower Cretaceous (Mannville) strata, Southwestern Alberta". Thesis, University of Oxford, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.371509.

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Libri sul tema "Jurassic stratigraphy":

1

International Congress on Jurassic Stratigraphy and Geology (4th 1994 Mendoza, Argentina). Advances in Jurassic research: 4th International Congress Jurassic Stratigraphy and Geology, Argentina, 1994. A cura di Riccardi A. C. Zurich-Uetikon, Switzerland: Transtec Publications Ltd., 1996.

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2

C, Riccardi A., International Union of Geological Sciences. Commission on Stratigraphy, International Subcommission on Jurassic Stratigraphy., Argentine Geological Society e International Congress on Jurassic Stratigraphy and Geology (4th : 1994 : Mendoza, Argentina), a cura di. Advances in Jurassic research: 4th International Congress on Jurassic Stratigraphy and Geology : Argentina, 1994. Zurich: Transtec, 1996.

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3

Cameron, B. E. B. Jurassic stratigraphy of the Queen Charlotte Islands, British Columbia. Ottawa, Ont., Canada: Geological Survey of Canada, 1985.

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4

Picard, Leo. The Jurassic stratigraphy in Israel and the adjacent countries. Jerusalem: Israel Academy of Sciences and Humanities, 1987.

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5

Canada, Geological Survey of. Jurassic Stratigraphy of the Queen Charlotte Islands, British Columbia. S.l: s.n, 1985.

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6

Lee, K. Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. Washington: U.S. G.P.O., 1989.

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7

Lee, K. Y. Triassic-Jurassic stratigraphy of the Culpeper and Barboursville basins, Virginia and Maryland. Washington, DC: Dept. of the Interior, 1989.

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8

Roberto, Colacicchi, Parisi Guido e Zamparelli Valeria, a cura di. Bioevents and integrate stratigraphy of the Triassic and the Jurassic in Italy. [Roma: Università "La Sapienza"], 1999.

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9

1962-, Arthur Andrew John, e Geological Survey of Canada, a cura di. Mesozoic stratigraphy and Jurassic paleontology west of Harrison Lake, southwestern British Columbia. Ottawa, Canada: Geological Survey of Canada, 1993.

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10

Stewart, John Harris. Triassic and Jurassic stratigraphy and paleogeography of west-central Nevada and eastern California. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1997.

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Capitoli di libri sul tema "Jurassic stratigraphy":

1

Frazier, William J., e David R. Schwimmer. "The Absaroka Sequence: Lower Pennsylvanian—Lower Jurassic". In Regional Stratigraphy of North America, 271–391. Boston, MA: Springer US, 1987. http://dx.doi.org/10.1007/978-1-4613-1795-1_7.

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Frazier, William J., e David R. Schwimmer. "The Zuni Sequence: Middle Jurassic—Upper Cretaceous". In Regional Stratigraphy of North America, 393–522. Boston, MA: Springer US, 1987. http://dx.doi.org/10.1007/978-1-4613-1795-1_8.

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3

Baumgartner, Peter O. "Sedimentary Stratigraphy and Paleogeographic Evolution". In Jurassic Sedimentary Evolution and Nappe Emplacement in the Argolis Peninsula (Peloponnesus, Greece), 19–83. Basel: Birkhäuser Basel, 1985. http://dx.doi.org/10.1007/978-3-0348-9319-0_5.

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4

Hallam, Anthony. "Major Bio-Events in the Triassic and Jurassic". In Global Events and Event Stratigraphy in the Phanerozoic, 265–83. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-79634-0_13.

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5

Mamilla, Venkateshwarlu. "Magnetic Polarity Stratigraphy Investigations of Middle-Upper Jurassic Sediments of Jara Dome, Kutch Basin, NW India". In Mesozoic Stratigraphy of India, 157–71. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-71370-6_5.

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Saha, Sandip, Shiladri S. Das e Subhronil Mondal. "Gastropod Biozonation for the Jurassic Sediments of Kutch and Jaisalmer Basins and Its Application in Interbasinal Correlation". In Mesozoic Stratigraphy of India, 333–72. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-71370-6_12.

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7

Halder, Kalyan. "Nautiloid Biostratigraphy of the Jurassic of Kutch, India: An Exploration of Bio- and Chrono-stratigraphic Potential of Nautiloids". In Mesozoic Stratigraphy of India, 291–309. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-71370-6_10.

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8

Dromart, G., S. Ferry e F. Atrops. "Allochthonous Deep-Water Carbonates and Relative Sea-Level Changes: The Upper Jurassic-Cretaceous of Southeast France". In Sequence Stratigraphy and Facies Associations, 295–305. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304015.ch16.

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Aurell, M., e A. Meléndez. "Sedimentary Evolution and Sequence Stratigraphy of the Upper Jurassic in the Central Iberian Chain, Northeast Spain". In Sequence Stratigraphy and Facies Associations, 343–68. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304015.ch18.

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10

Ren, Dong. "Jurassic-Cretaceous Non-Marine Stratigraphy and Entomofaunas in Northern China". In Rhythms of Insect Evolution, 1–16. Chichester, UK: John Wiley & Sons, Ltd, 2019. http://dx.doi.org/10.1002/9781119427957.ch1.

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Atti di convegni sul tema "Jurassic stratigraphy":

1

Gravestock, Christopher, Alex Bromhead, Mike Simmons, Frans Van Buchem e Roger Davies. "Stratigraphic Trap Potential in the Middle East – Examples from the Mesozoic". In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207229-ms.

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Abstract (sommario):

Abstract The Mesozoic stratigraphy of the Middle East is endowed with multiple world-class, economically significant petroleum systems. Since the first discovery of a major oilfield in an anticline structure in 1908 (Masjed-e-Suleyman, Iran), exploration and production in the Middle East has been largely focussed on relatively low-risk, large structural traps. However, across the Arabian Plate, unexplored structural traps at similar scales are becoming scarce. Therefore, in this mature petroleum province, attention must now focus on identifying the presence of subtle stratigraphic traps, especially within the hydrocarbon-rich Mesozoic stratigraphy. In order to locate and evaluate subtle stratigraphic traps, we have applied sequence stratigraphic principles across the Mesozoic strata of the Arabian Plate. This approach provides a regional, robust age-based framework which reduces lithostratigraphic uncertainty across international boundaries and offers predictive capabilities in the identification and extent of stratigraphic plays. Herein, we focus on three intervals of Mesozoic stratigraphy, namely Triassic, Middle-Late Jurassic and middle Cretaceous strata, in which regional sequence stratigraphic based correlations have identified stratigraphic trap potential. Each of these stratigraphic intervals are associated with the following stratigraphic traps:Triassic: Sub-crop traps associated with a base Jurassic regional unconformity and intra-Triassic unconformities. Onlap geometries associated with differential topography on the Arabian Plate.Middle-Late Jurassic: Pure stratigraphic trap geometries associated with basin margin progradation and pinch-out plays either side of the Rimthan Arch related to late Oxfordian/early Kimmeridgian sea-level fall.Middle Cretaceous: Sub-crop potential beneath the regional mid-Turonian unconformity, basin margin progradation and stratigraphic pinch-out geometries associated with onlap onto basin margins. This regional sequence stratigraphic approach highlights the remaining exploration and production opportunities within these hydrocarbon-rich stratigraphic intervals.

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Lucas, S. G. "Triassic-Jurassic stratigraphy in southwestern Colorado". In 68th Annual Fall Field Conference. New Mexico Geological Society, 2017. http://dx.doi.org/10.56577/ffc-68.149.

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3

Lucas, Spencer G., e Andrew B. Heckert. "Jurassic stratigraphy in west-central New Mexico". In 54th Annual Fall Field Conference. New Mexico Geological Society, 2003. http://dx.doi.org/10.56577/ffc-54.289.

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4

Agapitov, I. D., S. S. Kosova, S. G. Shilkin, A. A. Belova, A. V. Gorban e I. N. Kerusov. "Jurassic Sequence Stratigraphy of the Central Caspian Basin". In Geomodel 2017. Netherlands: EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201702216.

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5

Zverkov, N. G. "JURASSIC ICHTHYOSAURS OF SIBERIA AND THE ARCTIC". In PALEONTOLOGY, STRATIGRAPHY AND PALEOGEOGRAPHY OF THE MESOZOIC AND CENOZOIC IN BOREAL REGIONS. Trofimuk Institute of Petroleum Geology and Geophysics (SB RAS), 2021. http://dx.doi.org/10.18303/b978-5-4262-0104-0-80.

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6

Lucas, Spencer G., Adrian P. Hunt e Justin A. Spielmann. "Jurassic stratigraphy in the Chama Basin, northern New Mexico". In 56th Annual Fall Field Conference. New Mexico Geological Society, 2005. http://dx.doi.org/10.56577/ffc-56.182.

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Jongepier, K., J. Gjelberg e J. C. Rui. "Jurassic Stratigraphy and Sedimentology of the Southern Mid-Norwegian Shelf". In 57th EAEG Meeting. Netherlands: EAGE Publications BV, 1995. http://dx.doi.org/10.3997/2214-4609.201409670.

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Lucas, Spencer G., Orin J. Anderson e Clarence Pigman. "Jurassic stratigraphy in the Hagan Basin, north-central New Mexico". In 46th Annual Fall Field Conference. New Mexico Geological Society, 1995. http://dx.doi.org/10.56577/ffc-46.247.

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9

Rich, Adelaide, e Grant Shimer. "EARLY JURASSIC MOENAVE FORMATION STRATIGRAPHY AND PETROGRAPHY, CEDAR CITY, UTAH". In Joint 118th Annual Cordilleran/72nd Annual Rocky Mountain Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022cd-374190.

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Rogov, M. A. "EARLY JURASSIC GLENDONITES AND CLIMATE OF THE NORTHERN HEMISPHERE". In PALEONTOLOGY, STRATIGRAPHY AND PALEOGEOGRAPHY OF THE MESOZOIC AND CENOZOIC IN BOREAL REGIONS. Trofimuk Institute of Petroleum Geology and Geophysics (SB RAS), 2021. http://dx.doi.org/10.18303/b978-5-4262-0104-0-176.

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Rapporti di organizzazioni sul tema "Jurassic stratigraphy":

1

Poulton, T. P., W. K. Braun, M. M. Brooke e E. H. Davies. Jurassic [Chapter 4: Stratigraphy]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192366.

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Cameron, B. E. B., e H. W. Tipper. Jurassic stratigraphy of the Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120462.

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3

O'brien, J. Jurassic Stratigraphy of the Methow Trough, southwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120689.

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Poulton, T. P. Jurassic stratigraphy and fossil occurrences - Melville, Prince Patrick, and Borden Islands. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194021.

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Mahoney, J. B. Middle Jurassic stratigraphy of the Lillooet area, south-central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132811.

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6

Haggart, J. W. Progress in Jurassic and Cretaceous stratigraphy, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132826.

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7

Bringué, M., R. A. Fensome, T. P. Poulton, J M Galloway, J. P. Bujak, M L Golding, M. J. Orchard e G. L. Williams. The 2020 Canada datapack for TimeScale Creator: a new tool for Mesozoic - Cenozoic stratigraphy of the Canadian north. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/326099.

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Abstract (sommario):

The Geo-mapping for Energy and Minerals (GEM) program (2010-2020) provided a unique opportunity to advance the current level of understanding of the geological history of the Canadian North. In this contribution, based on the Trans-GEM Event Stratigraphy activity, a compilation of Mesozoic-Cenozoic stratigraphic data from across the GEM program regions and beyond is presented, with a focus on biostratigraphic events, using TimeScale Creator, a JAVA package that facilitates the compilation and comparison of large amounts of stratigraphic data while keeping track of changing absolute ages. The '2020 Canada datapack', which incorporates some information re-evaluated and refined from an earlier datapack, includes schemes using dinoflagellate cysts, spores and pollen, foraminifers and conodonts, and a new synthesis of Canadian Arctic Jurassic ammonite and Buchia bivalve biostratigraphy. This datapack will continue to be augmented after completion of the GEM program and will become a major tool in supporting an understanding of Canada's sedimentary basins, their resource potential and management.

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Embry, A. F. Uppermost triassic, jurassic, and lowermost cretaceous stratigraphy, Melville Island area, Arctic Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194020.

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9

Arthur, A. J., P. L. Smith, J. W. H. Monger e H. W. Tipper. Mesozoic stratigraphy and Jurassic paleontology west of Harrison Lake, southwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/183910.

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Poulton, T. P. Current Status of Jurassic Biostratigraphy and Stratigraphy, northern Yukon and Adjacent Mackenzie Delta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127560.

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