Bibliografías temáticas / Stratigraphic Proterozoic

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Literatura académica sobre el tema "Stratigraphic Proterozoic"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 25 de enero de 2023

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Artículos de revistas sobre el tema "Stratigraphic Proterozoic"

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Wu, He Yuan, and Bin Hao. "Third-Order Sequence Division of Yunmengshan and Baicaoping Formation of Proterozoic in Yuxi District of China: an Example from Xiatang Profile in Lushan." Advanced Materials Research 998-999 (July 2014): 1492–97. http://dx.doi.org/10.4028/www.scientific.net/amr.998-999.1492.

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There are controversies on the Proterozoic stratigraphic genesis, division, correlation and palaeogeographical evolution of western Henan in China. Based on the basic description of sedimentary facies, Yunmengshan and Baicaoping formation of Proterozoic typical section in western Henan is divided into 4 third-order sequences. Sequence stratigraphy framework which reflects sedimentary and overlap is established with basis of two kinds of facies-change surface and two kinds of diachrononism in stratigraphical records. Although chronostratigraphic belonging of Precambrian strata is controversial
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Halverson, Galen P., Susannah M. Porter, and Timothy M. Gibson. "Dating the late Proterozoic stratigraphic record." Emerging Topics in Life Sciences 2, no. 2 (July 13, 2018): 137–47. http://dx.doi.org/10.1042/etls20170167.

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The Tonian and Cryogenian periods (ca. 1000–635.5 Ma) witnessed important biological and climatic events, including diversification of eukaryotes, the rise of algae as primary producers, the origin of Metazoa, and a pair of Snowball Earth glaciations. The Tonian and Cryogenian will also be the next periods in the geological time scale to be formally defined. Time-calibrating this interval is essential for properly ordering and interpreting these events and establishing and testing hypotheses for paleoenvironmental change. Here, we briefly review the methods by which the Proterozoic time scale
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Sergeeva, Nina Dmitrievna, and Viktor Nikolaevich Puchkov. "REGIONAL STRATIGRAPHIC SCHEME OF THE UPPER AND FINAL RIPHEAN AND VENDIAN DEPOSITS OF THE SOUTHERN URALS (PROJECT 2022)." Geologicheskii vestnik, no. 2 (July 14, 2022): 3–14. http://dx.doi.org/10.31084/2619-0087/2022-2-1.

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The need to correct individual stratigraphic levels of the Regional Stratigraphic Scheme of the Upper Precambrian deposits of the Urals, existing since 1993, is due to the receipt of new data from lithological-stratigraphic, geotectonic and isotope-geochronological studies of the Upper Precambrian of the Southern Urals. Significant changes and clarifications in the stratigraphy of the Upper Precambrian formations of the region occurred in the Upper Riphean and Vendian of the Bashkir meganticlinorium in the Southern Urals, where the sections stratotypical for the Riphean and reference for the V
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Roscoe, S. M., and K. D. Card. "The reappearance of the Huronian in Wyoming: rifting and drifting of ancient continents." Canadian Journal of Earth Sciences 30, no. 12 (December 1, 1993): 2475–80. http://dx.doi.org/10.1139/e93-214.

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Striking stratigraphic and sedimentological similarities between the Early Proterozoic Huronian Supergroup of the Canadian Shield and the Snowy Pass Supergroup of Wyoming suggest that they were deposited in a single, broad, epicratonic basin developed atop a large Archean continent that included the Superior and Wyoming geological provinces. Breakup of the continent after the 2.2 Ga intrusion of widespread gabbro sheets and dykes resulted in the separation of the Archean Superior and Wyoming cratons and their Early Proterozoic covers. These crustal fragments were subsequently reassembled durin
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Martins-Neto, Marcelo A. "Sequence stratigraphic framework of Proterozoic successions in eastern Brazil." Marine and Petroleum Geology 26, no. 2 (February 2009): 163–76. http://dx.doi.org/10.1016/j.marpetgeo.2007.10.001.

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Phillips, Bruce J., Alan W. James, and Graeme M. Philip. "THE GEOLOGY AND HYDROCARBON POTENTIAL OF THE NORTH-WESTERN OFFICER BASIN." APPEA Journal 25, no. 1 (1985): 52. http://dx.doi.org/10.1071/aj84004.

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Recent petroleum exploration in EP 186 and EP 187 in the north-western Officer Basin has greatly increased knowledge of the regional stratigraphy, structure and petroleum prospectivity of the region. This exploration programme has involved the drilling of two deep stratigraphic wells (Dragoon 1 and Hussar 1) and the acquisition of 1438 km of seismic data. Integration of regional gravity and aeromagnetic data with regional seismic and well data reveals that the Gibson Sub-basin primarily contains a Proterozoic evaporitic sequence. In contrast, the Herbert Sub-basin contains a Late Proterozoic t
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Cook, Frederick A., and Samantha M. Siegel. "From Proterozoic strata to a synthesized seismic reflection trace: implications for regional seismic reflection patterns in northwestern Canada." Canadian Journal of Earth Sciences 43, no. 11 (November 1, 2006): 1639–51. http://dx.doi.org/10.1139/e06-040.

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Calculation of a synthetic seismic reflection trace from detailed descriptions of exposed Proterozoic strata in northwestern Canada permits correlation of reflections on regional seismic profiles to surface outcrop. Approximately 5.4 km (composite thickness) of Paleo- and Mesoproterozoic strata are exposed in the Muskwa anticlinorium that is located within the foreland of the Cordillera in northeastern British Columbia. The Tuchodi anticline is the easternmost structure of the Muskwa anticlinorium and has the deepest levels of Proterozoic strata exposed. At this location, prominent seismic ref
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Dub, S. A. "Upper Precambrian General Stratigraphic Scale of Russia: Main problems and proposals for improvement." LITHOSPHERE (Russia) 21, no. 4 (August 28, 2021): 449–68. http://dx.doi.org/10.24930/1681-9004-2021-21-4-449-468.

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Research subject. Main problems of the General Stratigraphic Scale (GSS) of the Upper Precambrian including uncertainties in the hierarchy of subdivisions are analyzed.Results. Prospects for detailing the Upper Precambrian GSS are discussed, along with questions of its correlation with International Chronostratigraphic Chart (ICSC) and establishing the lower boundaries of chronostratigraphic subdivisions. The importance of unifying the existing views is emphasized.Conclusions. It is proposed to carry out the following reforms of GSS: to abolish Acrothemes / Acrons; to approve the Proterozoic (
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Hiatt, Eric E., T. Kurtis Kyser, Paul A. Polito, Jim Marlatt, and Peir Pufahl. "The Paleoproterozoic Kombolgie Subgroup (1.8 Ga), McArthur Basin, Australia: Sequence stratigraphy, basin evolution, and unconformity-related uranium deposits following the Great Oxidation Event." Canadian Mineralogist 59, no. 5 (September 1, 2021): 1049–83. http://dx.doi.org/10.3749/canmin.2000102.

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ABSTRACT Proterozoic continental sedimentary basins contain a unique record of the evolving Earth in their sedimentology and stratigraphy and in the large-scale, redox-sensitive mineral deposits they host. The Paleoproterozoic (Stratherian) Kombolgie Basin, located on the Arnhem Land Plateau, Northern Territory, is an exceptionally well preserved, early part of the larger McArthur Basin in northern Australia. This intracratonic basin is filled with 1 to 2 km-thick, relatively undeformed, nearly flat-lying, siliciclastic rocks of the Kombolgie Subgroup. Numerous drill cores and outcrop exposure
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Ansdell, Kevin M., T. Kurtis Kyser, Mel R. Stauffer, and Garth Edwards. "Age and source of detrital zircons from the Missi Formation: a Proterozoic molasse deposit, Trans-Hudson Orogen, Canada." Canadian Journal of Earth Sciences 29, no. 12 (December 1, 1992): 2583–94. http://dx.doi.org/10.1139/e92-205.

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The Missi Formation in the Flin Flon Basin forms part of a discontinuous series of molasse-type sediments found throughout the Early Proterozoic Trans-Hudson Orogen in northern Saskatchewan and Manitoba. The Flin Flon Basin contains a sequence of proximal-fan to braided-stream fluvial conglomerates and sandstones, which unconformably overlie subaerially weathered Amisk Group volcanic rocks. Stratigraphic way-up indicators have been preserved, even though these rocks have undergone greenschist-facies metamorphism and polyphase deformation. The sedimentary rocks are crosscut by intrusive rocks,
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Tesis sobre el tema "Stratigraphic Proterozoic"

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Strauss, Toby Anthony Lavery. "The geology of the Proterozoic Haveri Au-Cu deposit, Southern Finland." Thesis, Rhodes University, 2004. http://hdl.handle.net/10962/d1015978.

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The Haveri Au-Cu deposit is located in southern Finland about 175 km north of Helsinki. It occurs on the northern edge of the continental island arc-type, volcano-sedimentary Tampere Schist Belt (TSB) within the Palaeoproterozoic Svecofennian Domain (2.0 – 1.75 Ga) of the Fennoscandian Shield. The 1.99 Ga Haveri Formation forms the base of the supracrustal stratigraphy consisting of metavolcanic pillow lavas and breccias passing upwards into intercalated metatuffs and metatuffites. There is a continuous gradation upwards from the predominantly volcaniclastic Haveri Formation into the overlying
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Baghiyan-Yazd, Mohammad Hassan. "Palaeoichnology of the terminal Proterozoic-Early Cambrian transition in central Australia : interregional correlation and palaeoecology." Title page, table of contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phb1445.pdf.

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Li, Longming, and 李龙明. "The crustal evolutionary history of the Cathaysia Block from the paleoproterozoic to mesozoic." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2010. http://hub.hku.hk/bib/B45693596.

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Zhao, Junhong, and 趙軍紅. "Geochemistry of neoproterozoic arc-related plutons in the Western margin of the Yangtze Block, South China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B40203748.

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Wang, Wei, and 王伟. "Sedimentology, geochronology and geochemistry of the proterozoic sedimentary rocks in the Yangtze Block, South China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2013. http://hdl.handle.net/10722/196033.

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The South China Craton comprises the Yangtze Block in the northwest and Cathaysia Block in the southeast. Located in the southeastern Yangtze Block, the Jiangnan Orogen formed through the amalgamation between the Yangtze and Cathaysia Blocks. The Yangtze Block has sporadically exposed Archean rocks in the north, Paleoproterozoic to Mesoproterozoic volcano-sedimentary sequences in the southwest and widespread Neoproterozoic sedimentary sequences accompanied by syn-sedimentary igneous rocks on the western and southeastern margins. The late Paleoproterozoic to early Mesoproterozoic Dongchuan, Da
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Swift, Peter Norton. "EARLY PROTEROZOIC TURBIDITE DEPOSITION AND MELANGE DEFORMATION, SOUTHEASTERN ARIZONA." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/187544.

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Greenschist-facies, Lower Proterozoic metasedimentary rocks of the Johnny Lyon Rills and Little Dragoon Mountains of southeastern Arizona were deposited prior to the intrusion of an approximately 1690 Ma rhyodacite pluton. Well-preserved primary structures indicate deposition by turbidity currents in an intermediate to neardistal setting. Sandstone compositions suggest derivation from either a complex, heterogeneous source or multiple source terranes that provided mature, quartzose sediment as well as lesser quantities of volcaniclastic detritus. Earliest deformation, predating both intrusion
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Baldim, Maurício Rigoni 1983. "O domo gnáissico Alto Alegre, transição embasamento-greenstone belt do Rio Itapicuru : evolução e significado tectônico." [s.n.], 2014. http://repositorio.unicamp.br/jspui/handle/REPOSIP/286596.

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Orientador: Elson Paiva de Oliveira<br>Dissertação (mestrado) - Universidade Estadual de Campinas, Instituto de Geociências<br>Made available in DSpace on 2018-08-26T10:50:20Z (GMT). No. of bitstreams: 1 Baldim_MauricioRigoni_M.pdf: 19163752 bytes, checksum: da3d83e0ed883c0984d79ed906f0528c (MD5) Previous issue date: 2014<br>Resumo: Domos gnáissicos são estruturas que podem estar associadas tanto aos orógenos extensionais quanto aos colisionais. Em orógenos colisionais, normalmente balizam os distintos terrenos dispondo-se em corredores estruturais. Na região nordeste do Cráton São Francisco
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Lane, Robert Andrew. "Geologic setting and petrology of the Proterozoic Ogilvie Mountains breccia of the Coal Creek inlier, southern Ogilvie Mountains, Yukon Territory." Thesis, University of British Columbia, 1990. http://hdl.handle.net/2429/29196.

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Ogilvie Mountains breccia (OMB) is in Early (?) to Late Proterozoic rocks of the Coal Creek Inlier, southern Ogilvie Mountains, Yukon Territory. Host rocks are the Wernecke Supergroup (Fairchild Lake, Quartet and Gillespie Lake groups) and lower Fifteenmile group. Distribution and cross-cutting relationships of the breccia were delineated by regional mapping. OMB was classified by clast type and matrix composition. Ogilvie Mountains breccia crops out discontinuously along two east-trending belts called the Northern Breccia Belt (NBB) and the Southern Breccia Belt (SBB). The NBB extends across
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Stewart, Kathryn. "High temperature felsic volcanism and the role of mantle magmas in proterozoic crustal growth : the Gawler Range volcanic province /." Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09PH/09phs8488.pdf.

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Harris, Charles William. "A sedimentological and structural analysis of the Proterozoic Uncompahgre Group, Needle Mountains, Colorado." Diss., Virginia Polytechnic Institute and State University, 1987. http://hdl.handle.net/10919/79644.

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Siliciclastic sediments of the Proterozoic Uncompahgre Group can be subdivided into stratigraphic units of quartzite (Q) and pelite (P); these units include a basal, fining- and thinning-upward retrogradational sequence (Q1-P1) that records the transition from an alluvial to a shallow-marine setting. Overlying the basal sequence are three thickening- and coarsening-upward progradational sequences (P2-Q2, P3-Q3 and P4-Q4) that were influenced by tide-, storm- and wave-processes. The progradational units are subdivided into the following facies associations in a vertical sequence. Outer-to inner
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Libros sobre el tema "Stratigraphic Proterozoic"

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1936-, Medaris L. G., and Geological Society of America, eds. Proterozoic geology: Selected papers from an International Proterozoic Symposium. Boulder, Colo: Geological Society of America, 1986.

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F, Gower Charles, Rivers Toby 1948-, Ryan Arthur Bruce 1951-, and Geological Association of Canada, eds. Mid-Proterozoic Laurentia-Baltica. St. John's, Nfld., Canada: Geological Association of Canada, Dept. of Earth Sciences, 1990.

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A, Kröner, and International Geological Congress (27th : 1984 : Moscow, Russia), eds. Proterozoic lithospheric evolution. Washington, D.C: American Geophysical Union, 1987.

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A, Grambling Jeffrey, Tewksbury Barbara J, and Geological Society of America. Rocky Mountain Section., eds. Proterozoic geology of the southern Rocky Mountains. Boulder, Colo: Geological Society of America, 1989.

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Blake, D. H., fl. 1967-, ed. Geology of the Proterozoic Davenport province, central Australia. Canberra: Australian Government Publishing Service, 1987.

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A, Winchester J., ed. Later Proterozoic stratigraphy of the northern Atlantic regions. Glasgow: Blackie, 1988.

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Dawes, Peter R. The Proterozoic Thule Supergroup, Greenland and Canada: History, lithostratigraphy, and development. Copenhagen, Denmark: Geological Survey of Denmark and Greenland, Ministry of Environment and Energy, 1997.

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Truswell, J. F. Early Proterozoic red beds on the Kaapvaal craton. Johannesburg: University of the Witwatersrand, 1990.

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Uppermost Proterozoic formations in central Mackenzie Mountains, Northwest Territories. Ottawa, Ont., Canada: Energy, Mines and Resources Canada, 1989.

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Greene, Robert C. Stratigraphy of the Late Proterozoic Murdama Group, Saudi Arabia. [Menlo Park, CA: U.S. Geological Survey], 1993.

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Capítulos de libros sobre el tema "Stratigraphic Proterozoic"

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Young, Grant M. "Earth's Earliest Extensive Glaciations: Tectonic Setting and Stratigraphic Context of Paleoproterozoic Glaciogenic Deposits." In The Extreme Proterozoic: Geology, Geochemistry, and Climate, 161–81. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/146gm13.

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van Aswegen, G., D. Strydom, W. P. Colliston, H. E. Praekelt, A. E. Schoch, H. J. Blignault, B. J. V. Botha, and S. W. van der Merwe. "The structural-stratigraphic development of part of the Namaqua metamorphic complex, South Africa—An example of Proterozoic major thrust tectonics." In Proterozic Lithospheric Evolution, 207–16. Washington, D. C.: American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd017p0207.

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Christie-Blick, Nicholas, and Marjorie Levy. "Stratigraphic and tectonic framework of Upper Proterozoic and Cambrian rocks in the western United States." In Late Proterozoic and Cambrian Tectonics, Sedimentation, and Record of Metazoan Radiation in the Western United States: Pocatello, Idaho, to Reno, Nevada 20–29 July, 1989, 7–21. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft331p0007.

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Frazier, William J., and David R. Schwimmer. "The Proterozoic." In Regional Stratigraphy of North America, 39–97. Boston, MA: Springer US, 1987. http://dx.doi.org/10.1007/978-1-4613-1795-1_3.

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Hibbard, James. "Stratigraphy of the Fleur de Lys Belt, northwest Newfoundland." In Later Proterozoic Stratigraphy of the Northern Atlantic Regions, 200–211. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4615-7344-9_16.

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Winchester, J. A. "Introduction." In Later Proterozoic Stratigraphy of the Northern Atlantic Regions, 1–13. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4615-7344-9_1.

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Gower, C. F. "The Double Mer Formation." In Later Proterozoic Stratigraphy of the Northern Atlantic Regions, 113–18. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4615-7344-9_10.

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Bentley, M. "The Colonsay Group." In Later Proterozoic Stratigraphy of the Northern Atlantic Regions, 119–30. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4615-7344-9_11.

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Winchester, J. A., and M. D. Max. "Pre-Dalradian rocks in NW Ireland." In Later Proterozoic Stratigraphy of the Northern Atlantic Regions, 131–45. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4615-7344-9_12.

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Winchester, J. A., and B. W. Glover. "The Grampian Group, Scotland." In Later Proterozoic Stratigraphy of the Northern Atlantic Regions, 146–61. Boston, MA: Springer US, 1988. http://dx.doi.org/10.1007/978-1-4615-7344-9_13.

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Actas de conferencias sobre el tema "Stratigraphic Proterozoic"

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Maloof, Adam, Ryan Manzuk, Emily C. Geyman, Akshay Mehra, Jaap A. Kaandorp, Mark Webster, Stacey Edmonsond, Bolton Howes, and Cedric Hagen. "FROM MODERN ANALOGS TO THREE DIMENSIONS: LESSONS LEARNED FOR INTERPRETING THE STRATIGRAPHIC RECORD OF THE PROTEROZOIC–PHANEROZOIC TRANSITION." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379218.

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Crombez, Vincent, Marcus Kunzmann, Claudio Delle Piane, Mohinudeen Faiz, Stuart Munday, and Anne Forbes. "STRATIGRAPHIC ARCHITECTURE OF A PROTEROZOIC SHALE PLAY: INSIGHTS FROM WELL CORRELATION IN THE VELKERRI FORMATION (BEETALOO SUB-BASIN, NORTHERN TERRITORY, AUSTRALIA)." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357071.

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Gorain, S., and A. Kumar. "Seismic-Sequence Stratigraphy and Paleo-Structure Analysis of Proterozoic Sediment within Ganga Basin, India." In 82nd EAGE Annual Conference & Exhibition. European Association of Geoscientists & Engineers, 2021. http://dx.doi.org/10.3997/2214-4609.202112620.

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Babu, Rupendra, and Veeru Kant Singh. "An Evaluation of Carbonaceous Metaphytic remains from the Proterozoic Singhora Group of Chhattisgarh Supergroup, India." In Proceedings of XXIII Indian Colloquium on Micropaleontalogy and Stratigraphy and International Symposium on Global Bioevents in Earth's History. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2013/63405.

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Informes sobre el tema "Stratigraphic Proterozoic"

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Lane, L. S., and R. B. MacNaughton. Central Foreland NATMAP Project: Proterozoic to Devonian stratigraphic sections in British Columbia and Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/299863.

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Cook, F. A. Lower Paleozoic and Proterozoic stratigraphy in the Colville Hills-Tweed Lake area, Northwest Territories: implications for regional seismic stratigraphic correlations. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132860.

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Lane, L. S., and R. B. MacNaughton. Introduction to stratigraphic sections from the Central Foreland NATMAP Project area: Proterozoic to Devonian successions. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/306301.

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Sevigny, J. H. Field and Stratigraphic Relations of Amphibolites in the Late Proterozoic Horsethief Creek Group, northern Adams River area, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122536.

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Wilton, D. H. C., C. S. MacDougall, L. M. Mackenzie, and C. Pumphrey. Stratigraphic and metallogenic relationships along the unconformity between Archean granite basement and the early Proterozoic Moran Lake Group, central Labrador. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122642.

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Aitken, J. D. Proterozoic Sedimentary Rocks [Chapter 4: Stratigraphy]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/192359.

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Bingham-Koslowski, N., L. T. Dafoe, M R St-Onge, E. C. Turner, J. W. Haggart, U. Gregersen, C. E. Keen, A. L. Bent, and J. C. Harrison. Introduction and summary. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321823.

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The papers contained in this bulletin provide a comprehensive summary and updated understanding of the onshore geology and evolution of Baffin Island, the Labrador-Baffin Seaway, and surrounding onshore regions. This introductory paper summarizes and links the geological and tectonic events that took place to develop the craton and subsequent Proterozoic to Cenozoic sedimentary basins. Specifically, the Precambrian and Paleozoic geology of Baffin Island and localized occurrences underlying the adjacent Labrador-Baffin Seaway, the Mesozoic to Cenozoic stratigraphy and rift history that records
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Cook, D. G., and B. C. MacLean. Subsurface Proterozoic stratigraphy and tectonics of the western plains of the Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215739.

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Mustard, P. S., C. F. Roots, and J. A. Donaldson. Stratigraphy of the Middle Proterozoic Gillespie Lake Group in the southern Wernecke Mountains, Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131367.

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McDonough, M. R., and P. S. Simony. Stratigraphy and structure of the late Proterozoic Miette Group, northern Selwyn Range, Rocky Mountains, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/122667.

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