Thematische Bibliographien / Jurassic-Cretaceous

Inhaltsverzeichnis

  1. Zeitschriftenartikel
  2. Dissertationen
  3. Bücher
  4. Buchteile
  5. Konferenzberichte
  6. Berichte der Organisationen

Auswahl der wissenschaftlichen Literatur zum Thema „Jurassic-Cretaceous“

Autor: Grafiati
Veröffentlicht am 8. November 2023

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Zeitschriftenartikel zum Thema "Jurassic-Cretaceous"

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Remane, Jürgen. "Jurassic-Cretaceous boundary." Geobios 27 (December 1994): 773. http://dx.doi.org/10.1016/s0016-6995(94)80246-7.

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Erdenetsogt, Bat-Orshikh. "Preliminary results of petroleum source rock evaluation of Mongolian Mesozoic oil shales." Геологийн асуудлууд 15 (February 23, 2023): 46–57. http://dx.doi.org/10.22353/.v15i01.2272.

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Jurassic and Cretaceous oil shale samples, collected from northern and central Mongolian basins, have been analyzed to determine their petroleum source rock potential. The contents of total organic carbon (TOC) and total sulfur, and source rock screening data were obtained by Rock-Eval pyrolysis. Cretaceous oil shales contain up to 17.4 wt.% TOC and Hydrogen Index (HI) values range from 638-957 mg HC/g TOC. Jurassic oil shale samples have similar TOC contents, ranging from 10.7 to 17.3 wt.%. HI values of Jurassic Tsagaan-Ovoo oil shale vary between 270-313 mg HC/g TOC. Average Tmax values of C
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Yin, Wei. "Hydrocarbon Geology Characteristics and Oil & Gas Resource Potential in the Afghan-Tajik Basin." Advanced Materials Research 734-737 (August 2013): 366–72. http://dx.doi.org/10.4028/www.scientific.net/amr.734-737.366.

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The Afghan-Tajik Basin is an intermontane depression between the mountain ranges of Gissar and Pamirs, and Jurassic system and Tertiary system are rich in large oil & gas resources. In order to assure sustainable supply of oil & gas from Central Asia, we deeply researched hydrocarbon geology characteristics and resource potentials. The basin belongs to paralic sedimentary environment, and develops 3 sedimentary strata: Jurassic, Cretaceous, and Tertiary. Afghan-Tajik Basin develops 3 main source rocks including clastic rocks of Jurassic, carbonate rocks of Cretaceous and mudstone rocks
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Sun, Shou-Liang, Shu-Wang Chen, Zhong-Jie Yang, et al. "Age of the Tuchengzi Formation in Western Liaoning Province and the Jurassic–Cretaceous Boundary from the Continuous Core Records of Well YD1, Jinyang Basin." Minerals 12, no. 8 (2022): 953. http://dx.doi.org/10.3390/min12080953.

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The Tuchengzi Formation is widely distributed in western Liaoning Province with a clear top and bottom. It is the focal area for the delineation of the terrestrial Jurassic–Cretaceous boundary in China. Based on continuous core samples taken from well YD1, detailed lithostratigraphic sequences and zircon uranium–lead (U-Pb) dating were used to investigate the Tuchengzi Formation. The zircon U-Pb ages of the tuff samples taken from the First and Third Members of the Tuchengzi Formation ranged from 153.8 to 137.16 Ma, indicating that they were formed in the late Middle Jurassic–Early Cretaceous.
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Mannion, Philip D. "A turiasaurian sauropod dinosaur from the Early Cretaceous Wealden Supergroup of the United Kingdom." PeerJ 7 (January 24, 2019): e6348. http://dx.doi.org/10.7717/peerj.6348.

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The Jurassic/Cretaceous (J/K) boundary, 145 million years ago, has long been recognised as an extinction event or faunal turnover for sauropod dinosaurs, with many ‘basal’ lineages disappearing. However, recently, a number of ‘extinct’ groups have been recognised in the Early Cretaceous, including diplodocids in Gondwana, and non-titanosauriform macronarians in Laurasia. Turiasauria, a clade of non-neosauropod eusauropods, was originally thought to have been restricted to the Late Jurassic of western Europe. However, its distribution has recently been extended to the Late Jurassic of Tanzania
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Bata, Timothy. "Evidences of Widespread Cretaceous Deep Weathering and Its Consequences: A Review." Earth Science Research 5, no. 2 (2016): 69. http://dx.doi.org/10.5539/esr.v5n2p69.

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This study highlights the effect of the Cretaceous greenhouse climate on weathering processes. Atmospheric CO2 level was relatively higher in the Cretaceous than it was in both the Jurassic and the Cenozoic. Consequently, temperature and humidity were higher in the Cretaceous than in the Jurassic and the Cenozoic. The interaction among the high levels of atmospheric CO2, extreme global warmth, and humidity in the Cretaceous resulted in widespread deep weathering. Cretaceous palaeo-weathering profiles are observed to occur at higher palaeolatitudes relative to the Jurassic and Cenozoic palaeo-w
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Jacobson, Carl E., César Jacques-Ayala, Andrew P. Barth, Juan Carlos García y Barragán, Jane N. Pedrick, and Joseph L. Wooden. "Protolith age of the Altar and Carnero complexes and latest Cretaceous–Miocene deformation in the Caborca–Altar region of northwestern Sonora, Mexico." Revista Mexicana de Ciencias Geológicas 36, no. 1 (2019): 95–109. http://dx.doi.org/10.22201/cgeo.20072902e.2019.1.784.

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In the Caborca–Altar area of northwest Sonora, variably deformed and metamorphosed sedimentary and volcanic rocks crop out in a northwest-southeast–trending belt (El Batamote belt) at least 70 km long. We obtained detrital zircon U-Pb ages from two distinctive components of the belt near Altar, here termed the Altar complex and Carnero complex. Zircon ages for metasandstone and metaconglomerate matrix from the Altar complex indicate a Late Cretaceous maximum age of sedimentation, with at least part of the complex no older than 77.5 ± 2.5 (2σ). Pre-Cretaceous detrital zircons in the complex wer
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Egebjerg Mogensen, Tommy, and John A. Korstgård. "Triassic and Jurassic transtension along part of the Sorgenfrei–Tornquist Zone in the Danish Kattegat." Geological Survey of Denmark and Greenland (GEUS) Bulletin 1 (October 28, 2003): 437–58. http://dx.doi.org/10.34194/geusb.v1.4680.

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In the Kattegat area, Denmark, the Sorgenfrei–Tornquist Zone, an old crustal weakness zone, was repeatedly reactivated during Triassic, Jurassic and Early Cretaceous times with dextral transtensional movements along the major boundary faults. These tectonic events were minor compared to the tectonic events of the Late Carboniferous – Early Permian and the Late Cretaceous – Early Tertiary, although a dynamic structural and stratigraphic analysis indicates that the Sorgenfrei–Tornquist Zone was active compared to the surrounding areas. At the end of the Palaeozoic, the area was a peneplain. Regi
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Ellis, G. K., A. Pitchford, and R. H. Bruce. "BARROW ISLAND OIL FIELD." APPEA Journal 39, no. 1 (1999): 158. http://dx.doi.org/10.1071/aj98011.

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The Barrow Island Field in the Barrow Sub-basin of the Carnarvon Basin was discovered in 1964 by West Australian Petroleum Pty Limited. It is the largest oil field in Western Australia. Appraisal drilling has defined in-place oil of 200 GL (1,250 MMBBL) and in-place gas of 16.5 Gm3 (580 BCF) primarily in the Lower Cretaceous Windalia Sand Member of the Muderong Shale and in- place gas of 14.5 Gm3 (515 BCF) in Middle Jurassic Biggada Formation. Additional hydrocarbon reservoirs have been discovered, including oil and gas in the Upper Jurassic Dupuy Formation, the Lower Cretaceous Malouet Format
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Zhimulev, F. I., E. V. Vetrov, I. S. Novikov, et al. "Mesozoic Intracontinental Orogeny in the Tectonic History of the Kolyvan’– Tomsk Folded Zone (Southern Siberia): a Synthesis of Geological Data and results of Apatite Fission Track Analysis." Russian Geology and Geophysics 62, no. 9 (2021): 1006–20. http://dx.doi.org/10.2113/rgg20204172.

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Abstract —The Kolyvan’–Tomsk folded zone (KTFZ) is a late Permian collisional orogen in the northwestern section of the Central Asian Orogenic Belt. The Mesozoic history of the KTFZ area includes Late Triassic–Early Jurassic and Late Jurassic–Early Cretaceous orogenic events. The earlier event produced narrow deep half-ramp basins filled with Early–Middle Jurassic molasse south of the KTFZ, and the later activity rejuvenated the Tomsk thrust fault, whereby the KTFZ Paleozoic rocks were thrust over the Early–Middle Jurassic basin sediments. The Mesozoic orogenic events induced erosion and the e
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Dissertationen zum Thema "Jurassic-Cretaceous"

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Woodfine, Richard Gareth. "Chemostratigraphy of Jurassic-cretaceous Italian carbonate platforms." Thesis, University of Oxford, 2002. http://ora.ox.ac.uk/objects/uuid:03c84d34-a27d-46fd-89b0-d69a1501d888.

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Samples of shallow-water carbonates were collected from Jurassic and Cretaceous Italian carbonate platforms and subjected to petrographic, diagenetic and chemostratigraphic analyses (<sup>87</sup>Sr/<sup>86</sup>Sr, δ<sup>13</sup>C<sub>carb</sub>, δ<sup>13</sup>C<sub>org</sub>, δ<sup>18</sup>O). In general, the new chemostratigraphic data generated reflect trends established by previous work, some of which has been carried out on biostratigraphically calibrated reference sections. Consequently, chemostratigraphic correlations (<sup>87</sup>Sr/<sup>86</sup>Sr, δ<sup>13</sup>C<sub>carb</sub>) of
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Jones, Charles Edward. "Strontium isotopes in Jurassic and Early Cretaceous seawater." Thesis, University of Oxford, 1992. http://ora.ox.ac.uk/objects/uuid:fe3733bd-8e31-4bba-a78b-6d8275a0075f.

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The collection and analysis of a large number of belemnites and oysters with excellent biostratigraphic and diagenetic control has resulted in a highly detailed determination of the seawater Sr-isotope curve through the Jurassic and Early Cretaceous. The new data confirm the broad trends established by previous work, but the much sharper resolution of the new data allows the application of Sr-isotope stratigraphy with an optimal stratigraphic resolution of ± 1 to 4 ammonite subzones (± 0.5 to 2 Ma). The data show a general decline from the Hettangian (Early Jurassic) to a minimum in the Callov
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Tennant, Jonathan. "The Jurassic/Cretaceous boundary : a hidden mass extinction in tetrapods?" Thesis, Imperial College London, 2016. http://hdl.handle.net/10044/1/44179.

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Reconstructing deep time trends in biodiversity remains a central goal for palaeobiologists, but our understanding of the magnitude and tempo of extinctions and radiations is confounded by uneven sampling of the fossil record. In particular, the Jurassic/Cretaceous (J/K) boundary, 145 million years ago, remains poorly understood. By applying a range of techniques for assessing changes in diversity, I demonstrate that both marine and non-marine tetrapod faunas show evidence for a protracted period of regional and global ecological and taxonomic reorganisation across the J/K boundary. Although m
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Currie, Brian Scott 1966. "Jurassic-Cretaceous evolution of the central Cordilleran foreland-basin system." Diss., The University of Arizona, 1998. http://hdl.handle.net/10150/282582.

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During Jurassic and Cretaceous time deposition in the western interior basin was controlled by a combination of subduction-related dynamic subsidence and thrust-generated flexural subsidence. Changes in the angle of oceanic plate subduction along the western margin of North America and thrust deformation in the Cordillera governed the spatial and temporal influences of these mechanisms throughout basin history. Dynamic subsidence was the primary control on basin deposition during Early-Middle Jurassic and Late Cretaceous time. During these periods, shallow-angle oceanic plate subduction beneat
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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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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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Smith, Giles A. "Palynology of the Jurassic/Cretaceous boundary interval in the Volga Basin, Russia." Thesis, University of Bristol, 1999. http://hdl.handle.net/1983/a981fc30-fa69-4cf5-aae5-7290d2a489df.

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Lott, Graham Keith. "Late Triassic, Jurassic and Early Cretaceous geology of the Southern North Sea Basin." Thesis, University of Leicester, 1985. http://hdl.handle.net/2381/8430.

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The primary aim of this thesis is to provide a comprehensive assessment of the geology of the Southern North Sea Basin during the Jurassic and Early Cretaceous. In order to achieve this the integration of a wide variety of data has been undertaken, including the interpretation of shallow seismic profiles, downhole geophysical log correlation and petrographic descriptions of all available core and seabed sample information from the offshore area. A number of onshore cored borehole sequences were examined in some detail to establish some control points with which to compare the largely uncored o
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Moreno, Karen. "Jurassic - Cretaceous dinosaur footprints from South America and pedal biomechanics in ornithopod dinosaurs." Thesis, University of Bristol, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.424417.

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Reis, Jonathan Hunter. "Jurassic and Cretaceous tectonic evolution of the southeast Castle Dome Mountains, southwest Arizona." [Ames, Iowa : Iowa State University], 2009.

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Bücher zum Thema "Jurassic-Cretaceous"

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H, Bate R., Wilkinson I. P, Thames Polytechnic. School of Earth Sciences., and British Micropalaeontological Society, eds. The Jurassic and Cretaceous of Eastern England. Thames Polytechnic, 1988.

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J, Hoedemaeker Ph. Correlation possibilities around the Jurassic/Cretaceous boundary. Rijksmuseum van Geologie en Mineralogie, 1987.

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Steuber, Thomas. Jurassic-Cretaceous Rudists (Mollusca, Hippuritacea): Bibliography 1758-1994. CPress, 1996.

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Rees, Jan. Jurassic and Early Cretaceous selachians--focus on southern Scandinavia. Lund University, 2001.

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Jurassic and Cretaceous floras and climates of the earth. Cambridge University Press, 1991.

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Howlett, P. J. Late Jurassic-early Cretaceous cephalopods of eastern Alexander Island, Antarctica. Palaeontological Association, 1989.

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Howlett, P. J. Late Jurassic-early Cretaceous cephalopods of eastern Alexander Island, Antarctica. Palaeontological Association, 1989.

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Challinor, A. B. Jurassic and Cretaceous Belemnitida of Misool archipelago, Irian Jaya, Indonesia. Republic of Indonesia, Ministry of Mines and Energy, Directorate General of Geology and Mineral Resources, Geological Research and Development Centre, 1989.

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Feldthusen, Jensen Thorkild, ed. Jurassic-Lower Cretaceous lithostratigraphic nomenclature for the Danish Central Trough. I kommission hos C.A. Reitzels forlag, 1986.

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Howlett, P. J. Late Jurassic-early Cretaceous cephalopods of Eastern Alexander Island, Antarctica. Palaeontological Association, 1989.

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Buchteile zum Thema "Jurassic-Cretaceous"

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Martín-Chivelet, Javier, José López-Gómez, Roque Aguado, et al. "The Late Jurassic–Early Cretaceous Rifting." In The Geology of Iberia: A Geodynamic Approach. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-11295-0_5.

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Yacobucci, Margaret M. "Macroevolution and Paleobiogeography of Jurassic-Cretaceous Ammonoids." In Topics in Geobiology. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-9633-0_8.

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

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Naqi, Mohammad, Ohood Alsalem, Suad Qabazard, and Fowzia Abdullah. "Petroleum Geology of Kuwait." In The Geology of Kuwait. Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-16727-0_6.

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AbstractKuwait has proven conventional oil reserves of about 100 billion barrels which makes it one of the major oil-producing countries worldwide. Most of this reserve is found in Cretaceous and Jurassic with minor quantities in the Paleogene sedimentary successions. Most hydrocarbon production comes from the siliciclastic Burgan Formation which is the most important reservoir in Kuwait. The Jurassic and Lower Cretaceous exhibit good quality source rocks that charged most of the hydrocarbon reservoirs in Kuwait and entered the oil window in Late Cretaceous to Eocene. Most of the hydrocarbon is trapped in very gentle four-way closure structures that are related to the deep-seated fault system of the Arabian Peninsula such as Khurais-Burgan Anticline. Hydrocarbon reservoirs in Kuwait are sealed and capped mainly by shale rocks and to a less extent by evaporites. In the last 15 years, Kuwait Oil Company (KOC) displayed interest in commercially exploiting unconventional hydrocarbon reserves and started laying significant emphasis on the exploration and development of unconventional resources. The aim of this work is to summarize the different petroleum systems of Kuwait including the Paleozoic, Mesozoic, and Cenozoic systems.
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Ren, Dong. "Jurassic-Cretaceous Non-Marine Stratigraphy and Entomofaunas in Northern China." In Rhythms of Insect Evolution. John Wiley & Sons, Ltd, 2019. http://dx.doi.org/10.1002/9781119427957.ch1.

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Iglesia Llanos, María Paula, and Diego A. Kietzmann. "Magnetostratigraphy of the Jurassic Through Lower Cretaceous in the Neuquén Basin." In Opening and Closure of the Neuquén Basin in the Southern Andes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29680-3_8.

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Shipley, Thomas H., Lewis J. Abrams, Yves Lancelot, and Roger L. Larson. "Late Jurassic-Early Cretaceous oceanic crust and early cretaceous volcanic sequences of the Nauru basin, western Pacific." In The Mesozoic Pacific: Geology, Tectonics, and Volcanism: A Volume in Memory of Sy Schlanger. American Geophysical Union, 1993. http://dx.doi.org/10.1029/gm077p0103.

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Salminen, Johanna, Jorge Dinis, and Octávio Mateus. "Preliminary Magnetostratigraphy for the Jurassic–Cretaceous Transition in Porto da Calada, Portugal." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_165.

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Nagy, Jenö, Magne Löfaldli, Sven A. Bäckström, and Halvor Johansen. "Agglutinated Foraminiferal Stratigraphy of Middle Jurassic to Basal Cretaceous Shales, Central Spitsbergen." In Paleoecology, Biostratigraphy, Paleoceanography and Taxonomy of Agglutinated Foraminifera. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-3350-0_38.

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Li, Jianguo. "Upper Jurassic and Lower Cretaceous Palynological Successions in the Qinghai-Xizang Plateau, China." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_229.

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Konferenzberichte zum Thema "Jurassic-Cretaceous"

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Pilskog, B., C. K. Siversen, and H. Emami. "Earliest Cretaceous-Late Jurassic of southern Rovuma Basin." In Third EAGE Eastern Africa Petroleum Geoscience Forum. EAGE Publications BV, 2017. http://dx.doi.org/10.3997/2214-4609.201702408.

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Trümpy, Daniel, Jan Witte, Immanuel Weber, and João P. Da Ponte Souza. "Source Rocks of Somalia – A Regional Assessment." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2582343-ms.

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ABSTRACT In total, some 60 wells have been drilled onshore and less than 10 offshore Somalia*, none of which in deep water. Several prospective basins remain undrilled, such as the offshore Jubba and Mid Somali High basins and the onshore Odewayne basin. In view of the gas discoveries offshore Mozambique and Tanzania, and also of encouraging results offshore Kenya (sub-commercial oil discovery Sunbird-1) and in Madagascar, the Somalian offshore and onshore basins were re-evaluated. As to the Somali onshore basins, the extension of the Yemeni Jurassic and Cretaceous rifts into Somalia highlight
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Qin, Guosheng, and Youjing Wang. "Jurassic Hydrocarbon System Appraisal and Implications for Prospectively in Central and Southern Iraq, Middle East." In ADIPEC. SPE, 2023. http://dx.doi.org/10.2118/216182-ms.

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The Jurassic hydrocarbon system in Middle East is one of the world's most important systems with several giant oilfields are discovered in Abu Dhabi, Saudi Arabia, etc[1–3]. The oil and gas discoveries of Jurassic formation are located in the northern part (Fig. 1). Such as the Najmah, Atrush, and Miran West oilfield in north Iraq. Meanwhile, it also considered the main producing reservoirs big reserve in adjacent countries. However, central and southern Iraq is an underexplored area due to large burial depth and limited data. Several wells have confirmed its huge potential. The appraisal of s
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"Mesozoic Tectonic Setting of SE Sundaland After Magmatism and Suture Evidences in JS-1 Ridge Area." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-14.

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Mesozoic plate convergence in SE Sundaland has been a source of debate for decades. A determination of plate convergence boundaries and timing have been explained in many publications, but not all boundaries were associated with magmatism. Through integration of both plate configurations and magmatic deposits, the basement can be accurately characterized over time and areal extents. This paper will discuss Cretaceous subductions and magmatic arc trends in SE Sundaland area with additional evidence found in JS-1 Ridge. At least three subduction trends are captured during the Mesozoic in the stu
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Vallejo, Cristian, Christian Romero, Brian K. Horton, and Janeth Gaibor. "JURASSIC TO EARLY CRETACEOUS TECTONOSTRATIGRAPHIC EVOLUTION OF EASTERN ECUADOR." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-341140.

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Galieva, M. F. "MODELS OF THE PALEOZOIC AND THE MESOZOIC FOCI OF HYDROCARBON GENERATION: ROLE IN FORMATION OF THE PRE-JURASSIC DEPOSITS WITHIN THE GERASIMOV FIELD (TOMSK REGION)." In All-Russian Youth Scientific Conference with the Participation of Foreign Scientists Trofimuk Readings - 2021. Novosibirsk State University, 2021. http://dx.doi.org/10.25205/978-5-4437-1251-2-193-195.

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This paper shows results of coupled paleotemperature modelling of sedimentary basins: «present» Jurassic-Cretaceous basin and Paleozoic «paleobasins» by an example of a section of well 12 belongs to the Gerasimov field within Tomsk Region. It is stated that Jurassic (Bazhenov) oil source and Paleozoic (Kehoreg) gas source are co-generating (by time of gen-eration, accumulation and conservation) for the reservoir of Inner Paleozoic.
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Sun, Ziming. "Structural Inversion, Reactivation and Extensional Detachment and Their Influence on the Formation and Preservation of Hydrocarbon Accumulations in Northern Western Desert of Egypt." In SPE/AAPG Africa Energy and Technology Conference. SPE, 2016. http://dx.doi.org/10.2118/afrc-2567052-ms.

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ABSTRACT The northern Western Desert Basins of Egypt experienced a complex evolutionary history and several transformation of tectonic stress field properties. An integrated analysis of geological and geophysical data reveals that structural inversion, reactivation and extensional detachment develop in the area, and have a significant effect on formation and preservation of hydrocarbon accumulations. Such an analysis is paramount for prospect evaluation, risk mitigation, and therefore improving the exploration success rate. The rifting in Jurassic and early Cretaceous formed several faulted-de
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8

Gradstein, Felix M., David K. Watkins, David K. Watkins, et al. "PLANKTONIC MICROFOSSIL EVOLUTION AND BIOSTRATIGRAPHY ACROSS THE JURASSIC-CRETACEOUS BOUNDARY." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-315472.

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9

van Laer, P., P. Nederlof, S. A. Ahsan, and F. Al Katheeri. "Northern Rub' Al-Khali Upper Jurassic – Lower Cretaceous Petroleum System." In Fourth Arabian Plate Geology Workshop. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142779.

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Grabowski, G. J., D. E. Sherrett, T. W. Jones, W. B. Maze, and J. Kendall. "Middle Jurassic to Early Cretaceous Petroleum Systems of the Arabian Plate." In Fourth Arabian Plate Geology Workshop. EAGE Publications BV, 2012. http://dx.doi.org/10.3997/2214-4609.20142778.

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Berichte der Organisationen zum Thema "Jurassic-Cretaceous"

1

Thomas, F. C., and R. A. Hasen. Fifteen hundred references for Jurassic and Lower Cretaceous forminifera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/130861.

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Thomas, F. C. The literature of Jurassic and early Cretaceous foraminifera - a compendium. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208915.

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3

Embry, A. F. New stratigraphic units, middle jurassic to lowermost cretaceous succession, Arctic Islands. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120253.

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4

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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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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6

Anderson, R. G. Jurassic and Cretaceous-Tertiary plutonic rocks on the Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122705.

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7

Williamson, M. A., and F. P. Agterberg. A quantitative foraminiferal correlation of the late Jurassic and early Cretaceous offshore Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/128094.

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8

Grinenko, V. S., A. V. Kostin, A. I. Kirichkova, and M. S. ZHelonkina. NEW DATA ON THE UPPER JURASSIC – LOWER CRETACEOUS ROCKS IN THE EASTERN SIBERIAN PLATFORM. ВЕСТНИК ВГУ, 2018. http://dx.doi.org/10.18411/vgu-sg-2018-2-48-55.

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9

Pe-Piper, G., B. Tsikouras, D. J. W. Piper, and S. Triantaphyllidis. Chemical fingerprinting of detrital minerals in the Upper Jurassic - Lower Cretaceous sandstones, Scotian Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2009. http://dx.doi.org/10.4095/248226.

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10

Kellett, D. A., and A. Zagorevski. Overlap assemblages: Laberge Group of the Whitehorse Trough, northern Canadian Cordillera. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/326064.

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The Laberge Group was deposited during the Early to Middle Jurassic in a marginal marine environment, in the northern Canadian Cordillera. It occurs as a narrow, elongated siliciclastic unit along more than 600 km of strike length, overlapping the Intermontane terranes of southern Yukon and northwestern British Columbia. The Laberge Group was deposited on the Late Triassic Stuhini and Lewes River groups, a volcano-plutonic complex of the Stikine terrane (Stikinia), and, locally, the Kutcho Arc. It is overlain by Middle Jurassic to Cretaceous clastic units. The variations in clast composition a
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