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Relevant bibliographies by topics / Middle Jurassic

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Academic literature on the topic 'Middle Jurassic'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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Journal articles on the topic "Middle Jurassic"

1

LUKASHEVICH, ELENA D. "Limoniidae (Diptera) in the Upper Jurassic of Shar Teg, Mongolia." Zoosymposia 3, no. 1 (2009): 131–54. http://dx.doi.org/10.11646/zoosymposia.3.1.12.

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A diverse Late Jurassic crane fly assemblage is described from Shar Teg locality (SW Mongolia), viz. Architipula krzeminskii n.sp., A. ampla n.sp., Mesotipula sigmoidea n.sp., ?M. brevicella n.sp., M. (Metatipula n.subgen.) continens n.sp., Tipunia undata n.sp., T. jorgi n.sp., Cretolimonia jurassica n.sp., C. pygmaea n. sp., Eotipulina sharategica n.sp., E. paula n.sp., E. evidens n.sp. and Eotipuloptera sp. The genus Praearchitipula Kalugina, 1985 is transferred to Pediciidae; it is the first Mesozoic record of this family (Middle Jurassic of Siberia). One species originally included in Prae

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Shi, Lu, Nan Ju, Yuhui Feng, Changqing Zheng, Yue Wu, and Xin Liu. "Petrogenesis and Tectonic Setting of the Early and Middle Jurassic Granitoids in the Chaihe Area, Central Great Xing’an Range, NE China." Minerals 13, no. 7 (2023): 917. http://dx.doi.org/10.3390/min13070917.

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To ascertain the Early-to-Middle Jurassic tectonic setting in the central Great Xing’an Range, this study investigated the Early and Middle Jurassic granitoids exposed in the Chaihe area in the central Great Xing’an Range based on isotopic chronology and petrogeochemistry. The results of this study show that the Early and Middle Jurassic granitoids have emplacement ages of 179–172 Ma. Moreover, the Early and Middle Jurassic granitoids are high-K calc-alkaline unfractionated I-type granitoids and high-K calc-alkaline fractionated I-type granitoids, respectively. The magma sources of the Early a

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Riccardi, Alberto C., Susana E. Damborenea, Miguel O. Manceñido, and Sara C. Ballent. "Middle Jurassic Biostratigraphyof Argentina." Geobios 27 (December 1994): 423–30. http://dx.doi.org/10.1016/s0016-6995(94)80163-0.

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XI-JIN, ZHAO, ROGER B. J. BENSON, STEPHEN L. BRUSATTE, and PHILIP J. CURRIE. "The postcranial skeleton ofMonolophosaurus jiangi(Dinosauria: Theropoda) from the Middle Jurassic of Xinjiang, China, and a review of Middle Jurassic Chinese theropods." Geological Magazine 147, no. 1 (2009): 13–27. http://dx.doi.org/10.1017/s0016756809990240.

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AbstractThe Middle Jurassic was a critical time in the evolution of theropod dinosaurs, highlighted by the origination and radiation of the large-bodied and morphologically diverse Tetanurae. Middle Jurassic tetanurans are rare but have been described from Europe, South America and China. In particular, China has yielded a number of potential basal tetanurans, but these have received little detailed treatment in the literature. Here we redescribe the postcranial skeleton of one of the most complete Chinese Middle Jurassic theropods,Monolophosaurus. Several features confirm the tetanuran affini

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DRUCKENMILLER, PATRICK S., and ERIN E. MAXWELL. "A Middle Jurassic (Bajocian) ophthalmosaurid (Reptilia, Ichthyosauria) from the Tuxedni Formation, Alaska and the early diversification of the clade." Geological Magazine 151, no. 1 (2013): 41–48. http://dx.doi.org/10.1017/s0016756813000125.

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AbstractOphthalmosauridae is a clade of derived thunniform ichthyosaurs that are best known from Callovian (late Middle Jurassic) to Cenomanian-aged (Late Cretaceous) deposits in both the Northern and Southern Hemispheres. Ophthalmosaurids arose prior to the Early–Middle Jurassic boundary, however, very little is known about their diversity and distribution in the earliest phase of their evolutionary history during the Aalenian–Bathonian (Middle Jurassic) interval. Here we describe new diagnostic ophthalmosaurid material from the Early Bajocian (Middle Jurassic) of Alaska. The specimen, UAMES

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ZHANG, KUIYAN, JINHUA LI, DING YANG, and DONG REN. "A new species of Archirhagio Rohdendorf, 1938 from the Middle Jurassic of Inner Mongolia of China (Diptera: Archisargidae)." Zootaxa 1984, no. 1 (2009): 61–65. http://dx.doi.org/10.11646/zootaxa.1984.1.4.

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The small genus Archirhagio Rohdendorf is an extinct Jurassic group of brachyceran flies. So far, only two known species have been found in the Middle/Upper Jurassic of Karatau (Kazakhstan) and the Middle Jurassic of Daohugou (Inner Mongolia, China) respectively. In this paper, a new species from the Middle Jurassic of Daohugou is described. A key to the species of the genus Archirhagio is given.

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Sajjadi Hezaveh, Freshteh, Firoozeh Hashemi Yazdi, Ali Khazaei, Navid Navidi-Izad, and Mohammad Taghi Badihagh. "Palynology of the Middle Jurassic strata from the Alborz Ranges, northwestern Iran." Boletín de la Sociedad Geológica Mexicana 77, no. 1 (2025): A141124. https://doi.org/10.18268/bsgm2025v77n1a141124.

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Palynomorphs are used for palynostratigraphy, and to derive paleoecological and paleobiogeographical inferences from the Middle Jurassic Shemshak Formation, Alborz Ranges, northwestern Iran. The rock unit contains diverse, reasonably preserved palynofloras dominated by miospores and dinoflagellate cysts. Vertical distribution of miospores allows for the introduction of Klukisporites variegatus -Striatella spp.- Contignisporites burgeri assemblage zone in the host strata. The presence of such key miospore species as Striatella jurassica, S. patenii, S. seebergensis, and Contignisporites burgeri

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Wang, Ping Li, Da Wei Lv, Hai Yan Liu, Xue Zheng, and Yu Lin Lv. "Migration Law of Mesozoic Qaidam Basin Depocenters." Advanced Materials Research 524-527 (May 2012): 63–66. http://dx.doi.org/10.4028/www.scientific.net/amr.524-527.63.

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According to stratigraphy and distribution features of the Qaidam Basin, and further the formation and migration of it’s depocenters, it is considered that the Middle-Upper Triassic were mainly sags scattered among the Qilian Mountains, the Alabasitao Mountains and the Kunlun Mountains; the Early Jurassic depocenters were located mainly in Lenghu depression and Yiliping sag at the northwest of the basin; several Middle Jurassic depocenters distributed from the northwest to the southeast of the basin along Sertengshan-Yuqia near front of the Qilian mountains; the Late Jurassic-Cretaceous depoce

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Xu, Zhongjie, Jintao Kong, Rihui Cheng, and Liaoliang Wang. "U–Pb dating of detrital zircons in the eastern Guangdong Basin, South China, and constraints on the tectonic transformation from the Early to Middle Jurassic." Canadian Journal of Earth Sciences 57, no. 4 (2020): 477–93. http://dx.doi.org/10.1139/cjes-2019-0050.

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Controversies exist regarding the mechanism of formation of basins located on the continental margin of South China as well as when they formed. It was ascertained based on clastic petrology, geochemical analysis, and zircon U–Pb dating that the sedimentary provenances in the eastern Guangdong Basin are mainly felsic igneous rocks from the late Early Jurassic to the Middle Jurassic. The late Early Jurassic Qiaoyuan Formation mainly shows major age peaks at approximately 238 Ma, 259 Ma, and 1858 Ma, and the Middle Jurassic Tangxia Formation shows major age peaks at approximately 169 Ma and 172

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Ahmad, Fayez. "Middle Jurassic brachiopod faunas from Northwestern Jordan." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2000, no. 5 (2000): 301–13. http://dx.doi.org/10.1127/njgpm/2000/2000/301.

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Dissertations / Theses on the topic "Middle Jurassic"

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Strogen, Dominic Paul. "Diagenesis of Middle to Upper Jurassic sandstones, East Greenland." Thesis, University of Reading, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.323408.

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Carter, Elizabeth Sibbald. "Early and middle Jurassic Radiolarian biostratigraphy, Queen Charlotte Islands, B.C." Thesis, University of British Columbia, 1985. http://hdl.handle.net/2429/24586.

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Radiolarian biostratigraphy is used to construct an informal zonation for sediments of upper Pliensbachian to lower Bajocian age from the Maude and Yakoun Formations, Queen Charlotte Islands, B.C. Paleoenvironmental studies assess depositional environment and the effects of changing facies relationships on the fauna. Seven distinctive assemblages are recognized comprising 167 species of spumellarian and nassellarian Radiolaria. The first well established middle Toarcian radiolarian assemblages are documented and both these and upper Toarcian assemblages are highly diverse and contain many new

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Vincent, Alastair James. "Palynofacies analysis of middle Jurassic sediments from the Inner Hebrides." Thesis, University of Newcastle Upon Tyne, 1995. http://hdl.handle.net/10443/979.

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A quantitative palynofacies study of thermally immature Middle Jurassic sediments of Skye, Raasay, and Eigg has been undertaken in order to examine kerogen and palynomorph distributions in relation to various potential controlling factors (lithology, lithofacies, depositional environment, sequence stratigraphy). This has involved performing rigorous kerogen and palynomorph counts on 440 samples from 12 localities (average sampling density 5 per metre in sampled sections), supported by 250 TOC and 57'Rock-Eval' pyrolysis analyses. The facies of the Middle Jurassic sediments of the Inner Hebride

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TANAKA, Shiro, Yusei KUROYANAGI, Kazuhiro SUZUKI, and Mamoru ADACHI. "Permo-Triassic and Early-Middle Jurassic granitoid clasts from the Jurassic conglomerates in the Mino terrane, central Japan." Dept. of Earth and Planetary Sciences, Nagoya University, 2002. http://hdl.handle.net/2237/2854.

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Brint, John Forsyth. "Isotope diagenesis and palaeofluid movement : Middle Jurassic Brent sandstones, North Sea." Thesis, University of Strathclyde, 1989. http://oleg.lib.strath.ac.uk:80/R/?func=dbin-jump-full&object_id=23310.

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The Middle North Sea, have simplified to a Jurassic deltaic Brent Group sandstones, northern complicated diagenetic sequence which may be kaolinite Fe,Ca carbonates - High porosities and Ness and Tarbert quartz overgrowths - Fe,Mg carbonates - illite. existed in the Etive, throughout diagenesis. By permeabilities have Formation sandstones contrast, the highly micaceous and r,elatively finer grained Rannach Formation sandstones have good porosities but very poor permeabilities due to burial compaction and carbonate cementation. Oxygen and hydrogen isotope studies indicate that early diagenesis

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Norris, Michelle Samantha. "A facies analysis of Middle-Upper Jurassic boundary beds in Europe." Thesis, University of Birmingham, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.539902.

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A facies analysis of Middle-Upper Jurassic boundary beds, i.e. Callovian-Oxfordian Stage boundary beds, has been carried out on numerous sections across Europe, with the aim of constructing relative sea-level curves for each geographic area. Accurate correlation of the various epeiric-sea, sedimentary successions has been achieved using ammonite zonations. The comparison of twelve relative sea-level curves has led to the recognition of regional sea-level events in Europe during the Callovian-Early Oxfordian interval. A regional sea-level rise occurred during the Middle and Late Callovian, reac

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Greenwood, Peter Jeremy. "Diagenesis of Middle Jurassic sandstones and mud rocks, Brae area, North Sea." Thesis, Imperial College London, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.294999.

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Ploynoi, Manwika Parcell William C. "Development of middle Jurassic microbial buildups in the Bighorn Basin of northern Wyoming." Diss., A link to full text of this thesis in SOAR, 2007. http://soar.wichita.edu/dspace/handle/10057/1150.

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Thesis (M.S.)--Wichita State University, College of Liberal Arts and Sciences, Dept. of Geology.<br>"May 2007." Title from PDF title page (viewed on Dec. 27, 2007). Thesis adviser: William C. Parcell. Includes bibliographic references (leaves 73-77).

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Corbett, Patrick W. M. "Reservoir characterisation of a laminated sediment : the Rannoch Formation, Middle Jurassic, North Sea." Thesis, Heriot-Watt University, 1993. http://hdl.handle.net/10399/1435.

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The probe permeameter is a recently developed device providing a small scale measurement of permeability. About 15,000 probe permeameter measurements were acquired for analysis during this study. These data were acquired by Statoil from cores in two North Sea wells. These cores are from the Middle Iurassic Rannoch Formation of the Brent Group. This reservoir unit was selected for this study because of its laminated nature and challenge to conventional description and simulation practice. All aspects of probe permearnetry are investigated in this study; the volume of investigation, the compatib

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Noe`, Leslie Francis. "A taxonomic and functional study of the Callovian (Middle Jurassic) Pliosauroidea (Reptilia, Sauropterygia)." Thesis, University of Derby, 2001. http://hdl.handle.net/10545/211770.

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The short-snouted Callovian pliosaurs, Liopleurodon ferox SAUVAGE 1873, Simolestes vorax ANDREWS 1909 and Pachycostasaurus dawni CRUICKSHANK, MARTILL and NOE 1996, of the Peterborough Member, Oxford Clay Formation are of considerable palaeontological importance. The restricted geographical and temporal range, exceptional preservation, relative abundance, and easy removal of matrix, make the Callovian pliosaurs excellent subjects for detailed study. Skull material is known from all Callovianpliosaurs, but has been little studied, and much excellent material remains undescribed. The taxonomy of

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Books on the topic "Middle Jurassic"

1

Cox, B. M. English Callovian (Middle Jurassic) perisphinctid ammonites. Palaeontographical Society, 1988.

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Cox, B. M. English Callovian (Middle Jurassic) perisphinctid ammonites. Palaeontographical Society, 1988.

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3

Imlay, Ralph Willard. Early and middle Bajocian (middle Jurassic) ammonites from southern Alaska. U.S. G.P.O., 1985.

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4

Moon, Benjamin C. Ichthyosaurs of the British Middle and Upper Jurassic. The Palaeontographical Society, 2016.

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5

Wakefield, M. I. Middle Jurassic (Bathonian) ostracoda from the Inner Hebrides, Scotland. Palaeontographical Society, 1994.

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Sumbler, M. G. The Lincolnshire limestone formation (Middle Jurassic) near Grantham, Lincolnshire. British Sedimentological Research Group, 1991.

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Guthrie, Gregory M. Pre-Middle Jurassic rocks beneath the Alabama Gulf Coastal Plain. Geological Survey of Alabama, Stratigraphy and Paleontology Division, 1992.

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8

Dybkjær, Karen. Palynological zonation and palynofacies investigation of the Fjerritslev Formation (Lower Jurassic-basal Middle Jurassic) in the Danish Subbasin. Danmarks geologiske undersøgelse, 1991.

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Norris, Michelle Samantha. A facies analysis of Middle-Upper Jurassic boundary beds in Europe. University of Birmingham, 1993.

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10

International Association of Radiolarian Paleontologists and INTERRAD Jurassic-Cretaceous Working Group, eds. Middle Jurassic to Lower Cretaceous radiolaria of Tethys: Occurences, systematics, biochronology. Section des Sciences de la Terre, Université de Lausanne, 1995.

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Book chapters on the topic "Middle Jurassic"

1

Wang, Huiji, and Shengqiu Yang. "Middle Jurassic Gastropods from Xizang (Tibet), China." In Palaeontologia Cathayana. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-662-12662-2_7.

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Ballent, Sara C. "Lower and Middle Jurassic Ostracoda from Argentina." In Ostracoda and Global Events. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-1838-2_15.

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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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Gómez, Juan José, Roque Aguado, Ana Cristina Azerêdo, et al. "The Late Triassic–Middle Jurassic Passive Margin Stage." In The Geology of Iberia: A Geodynamic Approach. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-11295-0_4.

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Khain, V. E., A. N. Balukhovsky, and K. B. Seslavinsky. "Middle Triassic to Middle Jurassic: Eve of Break-up of Pangaea II." In Historical Geotectonics. Routledge, 2021. http://dx.doi.org/10.1201/9780203751855-1.

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RAVNÅS, RODMAR, KARI BERGE, HEATHER CAMPBELL, CRAIG HARVEY, and MIKE J. NORTON. "Halten Terrace Lower and Middle Jurassic inter-rift megasequence analysis." In From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin. John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118920435.ch10.

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Ravenne, C., A. Galli, H. Beucher, R. Eschard, D. Guerillot, and Heresim Group. "Outcrop Studies and Geostatistical Modelling of a Middle Jurassic Brent Analogue." In The European Oil and Gas Conference. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-010-9844-1_72.

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Hirsch, Francis, Howard R. Feldman, Fayez Ahmad, Mena Schemm-Gregory, and Mark A. Wilson. "Correlation of the Middle Jurassic (Callovian) Formations Across the Dead Sea Rift." In Springer Geology. Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-04364-7_126.

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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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Massari, Francesco, and Hildegard Westphal. "Microbialites in the Middle–Upper Jurassic Ammonitico Rosso of the Southern Alps (Italy)." In Cellular Origin, Life in Extreme Habitats and Astrobiology. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-0397-1_10.

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Conference papers on the topic "Middle Jurassic"

1

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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Kavoosi, M. A., M. Sepehr, and S. Sherkati. "Kopet-Dagh Basin Evolution During Middle-late Jurassic." In 1st International Petroleum Conference and Exhibition Shiraz 2009. EAGE Publications BV, 2009. http://dx.doi.org/10.3997/2214-4609.20145873.

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Yousif, Samir, and Ghalib Nouman. "Geological Model Of The Jurassic Section In The State Of Kuwait." In Middle East Oil Show. Society of Petroleum Engineers, 1995. http://dx.doi.org/10.2118/29796-ms.

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Hu, J., J. Witte, and F. A. Neves. "Regional Characterization of Middle Triassic-Middle Jurassic Tight Reservoirs in Abu Dhabi, UAE." In Third EAGE/AAPG Workshop on Tight Reservoirs in the Middle East. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201414107.

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Wilson, E. N. "Evaluation of Jurassic Arab D Reservoir Quality in Low-Relief Traps in Qatar." In Middle East Oil Show. Society of Petroleum Engineers, 1991. http://dx.doi.org/10.2118/21447-ms.

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Hassan, T. H. "The Lower and Middle Jurassic in Offshore Abu Dhabi: Stratigraphy and Hydrocarbon Occurrence." In Middle East Oil Show. Society of Petroleum Engineers, 1989. http://dx.doi.org/10.2118/18011-ms.

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Toland, Christopher, R. G. Peebles, and G. M. Walkden. "Upper Jurassic and Basal Cretaceous Outcrop Sequence Stratigraphy of Wadi Hagil, Ras Al Khaimah." In Middle East Oil Show. Society of Petroleum Engineers, 1993. http://dx.doi.org/10.2118/25581-ms.

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Ruiz, Daniel, Daniel F. Stockli, and Elisa Fitz-Diaz. "EARLY TO MIDDLE JURASSIC JURASSIC RIFTING IN SOUTHEAST MEXICO AND IMPLICATIONS FOR GULF OF MEXICO OPENING." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380561.

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Al-Dousari, Sara, Haifa Al-Bader, Ahmed Al-Otaibi, Sara Al-Shuaib, and Bahaskar Chakrabarti. "Significant Impact of Non H-C Gases (NHG) on Reservoir Fluid of a Jurassic, HPHT and Tight Carbonate Discovery in North of Kuwait: A Case Study of a Sour and Critical Fluid Characteristics and Fluid Compartmentalization." In Middle East Oil, Gas and Geosciences Show. SPE, 2023. http://dx.doi.org/10.2118/213472-ms.

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Abstract The objective of this paper is to show the effect of non-HC gases NHG on critical fluid characterization of HPHT discovered deep Jurassic reservoir in north Kuwait in addition to Fluid characterization and compartmentalization with objective of assessing HC potential, well deliverability and reservoir fluid & rock characteristics. Jurassic reservoirs in the state of Kuwait are deep and tight with High-Pressure and High-Temperature (HPHT) environment. The discovery well was drilled targeting the Marrat formation to prove hydrocarbon in this area. The well was successfully completed

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Kimbrough, David L. "MIDDLE JURASSIC CORDILLERAN ARC FLARE-UP AND BAJOCIAN ENVIRONMENTAL IMPACT." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-332926.

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Reports on the topic "Middle Jurassic"

1

Monger, J. W. H., J. O. Wheeler, H. W. Tipper, et al. Cordilleran Terranes [Chapter 8: Upper Devonian To Middle Jurassic Assemblages]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134091.

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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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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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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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Gordey, S. P., H. H. J. Geldsetzer, D. W. Morrow, et al. Ancestral North America [Chapter 8: Upper Devonian To Middle Jurassic Assemblages]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/134089.

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Wilson, R. C. L. A Reconnaissance Sedimentological Study of the Middle Jurassic Shaunavon Formation, southwestern Saskatchewan. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/130159.

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Ricketts, B. D., and C. A. Evenchick. Analysis of the Middle To Upper Jurassic Bowser Basin, northern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132498.

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Brown, R. L., V. J. McNicoll, R. R. Parrish, and R. J. Scammell. Middle Jurassic Plutonism in the Kootenay Terrane, northern Selkirk Mountains, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132918.

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Poulton, T. P., R. L. Hall, H. W. Tipper, B. E. B. Cameron, and E S Carter. Current Status of Middle Jurassic Biostratigraphy of the Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/131973.

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Haggart, J. W. New Sections of Yakoun Group [Middle Jurassic] Strata, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132533.

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