Готові списки джерел за темами / Late Proterozoic

Добірка наукової літератури з теми "Late Proterozoic"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 29 січня 2023

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Статті в журналах з теми "Late Proterozoic"

1

Chumakov, N. M. "Late Proterozoic African glacial era." Stratigraphy and Geological Correlation 19, no. 1 (February 2011): 1–20. http://dx.doi.org/10.1134/s0869593810061012.

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2

Hambrey, M. J., and W. B. Harland. "The late proterozoic glacial era." Palaeogeography, Palaeoclimatology, Palaeoecology 51, no. 1-4 (October 1985): 255–72. http://dx.doi.org/10.1016/0031-0182(85)90088-4.

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3

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 is dated and provide an up-to-date compilation of age constraints on key fossil first and last appearances, geological events, and horizons during the Tonian and Cryogenian periods. We also develop a new age model for a ca. 819–740 Ma composite section in Svalbard, which is unusually complete and contains a rich Tonian fossil archive. This model provides useful preliminary age estimates for the Tonian succession in Svalbard and distinct carbon isotope anomalies that can be globally correlated and used as an indirect dating tool.
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4

Brookfield, M. E. "Lithostratigraphic correlation of Blaini Formation (late Proterozoic, Lesser Himalaya, India) with other late Proterozoic tillite sequences." Geologische Rundschau 76, no. 2 (June 1987): 477–84. http://dx.doi.org/10.1007/bf01821087.

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5

Jepsen, H. F., J. C. Escher, J. D. Friderichsen, and A. K. Higgins. "The geology of the north-eastern corner of Greenland - photogeological studies and 1993 field work." Rapport Grønlands Geologiske Undersøgelse 161 (January 1, 1994): 21–33. http://dx.doi.org/10.34194/rapggu.v161.8240.

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Late Archaean and Early Proterozoic crust-forming events in North-East and eastern North Greenland were succeeded by Middle Proterozoic sedimentation and volcanic activity; Late Proterozoic through Tertiary sedimentation was interrupted by several periods of tectonic activity, including the Caledonian orogeny in East Greenland and the Mesozoic deformation of the Wandel Hav mobile belt. Photogeological studies helped pinpoint areas of special interest which were investigated during the short 1993 field season. Insights gained during field work include: the nature of the crystalline basement terrain in the Caledonian fold belt, redefinition of the upper boundary of the Upper Proterozoic Rivieradal sandstones, revision of Caledonian nappe terminology, and the northern extension of the Caledonian Storstrømmen shear zone.
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6

Carver, J. H., and I. M. Vardavas. "Precambrian glaciations and the evolution of the atmosphere." Annales Geophysicae 12, no. 7 (June 30, 1994): 674–82. http://dx.doi.org/10.1007/s00585-994-0674-3.

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Abstract. Precambrian glaciations appear to be confined to two periods, one in the early Proterozoic between 2.5 and 2 Gyears BP (Before Present) and the other in the late Proterozoic between 1 and 0.57 Gyear BP. Possible reasons for these broad features of the Precambrian climate have been investigated using a simple model for the mean surface temperature of the Earth that partially compensates for the evolution of the Sun by variations in the atmospheric CO2 content caused by outgassing, the formation of continents and the weathering of the Earth's land surface. It is shown that the model can explain the main changes in the Precambrian climate if the early Proterozoic glaciations were caused by a major episode of continental land building commencing about 3 Gyears BP while the late Proterozoic glaciations resulted from biologicallyenhanced weathering of the land surface due to the proliferation of life forms in the transition from the Proterozoic to the Phanerozoic that began about 1 Gyear BP.
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7

Serezhnikova, E. A. "Skeletogenesis in problematic Late Proterozoic Lower Metazoa." Paleontological Journal 48, no. 14 (December 2014): 1457–72. http://dx.doi.org/10.1134/s0031030114140123.

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Al-Fugha, Hassan. "Petrology and petrogenesis of a Late Proterozoic dyke swarm in South-Jordan." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 2002, no. 4 (April 25, 2002): 201–19. http://dx.doi.org/10.1127/njgpm/2002/2002/201.

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Clark, G. S., and D. C. P. Schledewitz. "Rubidium–strontium ages of Archean and Proterozoic rocks in the Nejanilini and Great Island domains, Churchill Province, northern Manitoba, Canada." Canadian Journal of Earth Sciences 25, no. 2 (February 1, 1988): 246–54. http://dx.doi.org/10.1139/e88-027.

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Rubidium–strontium whole-rock ages are reported from the Nejanilini – Great Island area in northeastern Manitoba. This area is part of an extensive zone of Archean basement that was metamorphosed and intruded by granitic magma during the Proterozoic; it extends into Saskatchewan and southern District of Keewatin, Northwest Tertitories. An age of 2577 ± 42 Ma (1σ error) for the extensive Nejanilini granulite massif (Nejanilini domain), considered one of the oldest rock units in the area, is interpreted as a minimum age for late Archean granulite-facies metamorphism. A minimum age of 2052 ± 41 Ma (initial ratio 0.7150) for quartz–feldspar porphyry that intrudes the Seal River volcanic suite constrains the age of these volcanics and could represent a partially reset Archean age. Early Proterozoic quartzite and metagreywacke of the Great Island Group unconformably overlies the quartz–feldspar porphyry. These metasedimentary rocks, which are probably correlative with the Daly Lake Group (Saskatchewan) or the Hurwitz Group (southern District of Keewatin), give an age of 1885 ± 85 Ma, with an initial ratio of 0.7093. The age records the time of closure of the Rb–Sr isotopic system subsequent to early Proterozoic metamorphism. The age and initial ratio are consistent with published results for other, possibly correlative, metasedimentary rocks in this zone. Modelling the Rb–Sr isotopic data constrains the time of sedimentation to between ca. 2100 and 2000 Ma ago. Syn- to late-kinematic, early Proterozoic granite to granodiorite batholiths, which intruded metasedimentary rocks of the Great Island Group, may largely be the product of melting of Archean basement, based on field evidence and high initial 87Sr/86Sr ratios. The Caribou Lake porphyritic quartz monzonite gives an age of 1795 ± 35 Ma, with an initial 87Sr/86Sr ratio of 0.7084. High initial ratios seem to typify early Proterozoic granitic rocks in this remobilized craton.
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10

Bertrand, Jean Michel, and Emmanuel Ferraz Jardim de Sá. "Where are the Eburnian–Transamazonian collisional belts?" Canadian Journal of Earth Sciences 27, no. 10 (October 1, 1990): 1382–93. http://dx.doi.org/10.1139/e90-148.

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The reconstruction of Early Proterozoic crustal evolution and geodynamic environments, in Africa and South America, is incomplete if cratonic areas alone are studied. If the presence of high-grade gneisses is considered as a first clue to past collisional behaviour, 2 Ga high-grade gneisses are more abundant within the Pan-African–Brasiliano mobile belts than in the intervening pre-Late Proterozoic cratons. The West African craton and the Guiana–Amazonia craton consist of relatively small Archaean nuclei and widespread low- to medium-grade volcanic and volcanoclastic formations intruded by Early Proterozoic granites. By contrast, 2 Ga granulitic assemblages and (or) nappes and syntectonic granites are known in several areas within the Pan-African–Brasiliano belts of Hoggar–Iforas–Air, Nigeria, Cameroon, and northeast Brazil. Nappe tectonics have been also described in the Congo–Chaillu craton, and Early Proterozoic reworking of older granulites may have occurred in the São Francisco craton. The location of the Pan-African–Brasiliano orogenic belts is probably controlled by preexisting major structures inherited from the Early Proterozoic. High-grade, lower crustal assemblages 2 Ga old have been uplifted or overthrust and now form polycyclic domains in these younger orogenic belts, though rarely in the cratons themselves. The Congo–Chaillu and perhaps the São Francisco craton are exceptional in showing controversial evidence of collisional Eburnian–Transamazonian assemblages undisturbed during Late Proterozoic time.
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Дисертації з теми "Late Proterozoic"

1

Phillips, Johnnie O. "Petrology of the Late Proterozoic(?) - Early Cambrian Arumbera Sandstone and the Late Proterozoic Quandong Conglomerate, East-central Amadeus Basin, Central Australia." DigitalCommons@USU, 1986. https://digitalcommons.usu.edu/etd/6684.

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Throughout the James Ranges and Gardiner Range the Arumbera Sandstone forms prominent strike ridges with distinctive dark reddish slopes and pale red to orange-white cliffs. Because of their lithologic and stratigraphic similarities, the names Eninta and ''Quandong" for these units should be suppressed in favor of the name of Arumbera Sandstone, which has precedence. The stratigraphic and lithologic differences observed between the Quandong Conglomerate in the type locality and the Arumbera Sandstone in the study area suggest that these units are not equivalent. Similarites with the Areyonga Formation suggest the Quandong Conglomerate could be part of the Areyonga Formation. Lithofacies la, ld, and 2b, and Unit 3 of the Arumbera and its equivalents are typically recessive arkoses, subarkose, and mudrocks. They are interpreted as nearshore-marine to coastal deltaic deposits which include intertonguing tidal-flat, tidal-channel, and beach sediments. Lithofacies 1b and 2a consist of cliff-forming arkoses, subarkoses, and lithic arkoses. Lithofacies 2c is also resistant, and consists of orthoconglomerates and conglomeratic sandstones. Lithofacies 1e is moderately resistant, and consists of paraconglomerates, conglomeratic sandstones, and mudrocks. It and lithofacies 2c contain pebbles and small cobbles of chert, quartzite, vein quartz, silicified ooids, and limestone, dolostone, shale, and sandstone. These four lithofacies are interpreted as braidplain and fluvial sheet sands. In the east-central part of the Amadeus Basin the Arumbera Sandstone probably was deposited in a coastal environment as a sequence of deltaic sediments that was dominated by fluvial processes. The Arumbera Sandstone appears to be the molasse derived from the Late Proterozoic and Early Cambrian Petermann Ranges orogeny. Source rocks include sedimentary, low- to middle-rank metamorphic, and plutonic granites. Grain mineralogy and weathering characteristics suggest a hot, semiarid climate during deposition of the Arumbera. The Arumbera Sandstone and Quandong Conglomerate contain fair to good porosity and permeability, and petrographic evidence shows mesogenetic generation of secondary porosity. Previous and present burial depths are adequate for the generation of petroleum. The presence of suitable underlying .source rocks, overlying salt of the Chandler for a seal, and stratigraphic and structural traps suggest a good potential for petroleum. Production of dry gas from the lower part of the Arumbera at Dingo field, north of Deep Well Homestead, confirms the petroleum potential of this formation.
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2

Teitz, Martin W. "Late proterozoic Yellowhead and Astoria Carbonate Platforms, southwest of Jasper, Alberta." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63371.

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3

Haines, Peter W. "Carbonate shelf and basin sedimentation, late Proterozoic Wonoka Formation, South Australia /." Title page, contents and summary only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phh152.pdf.

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Smith, Peter B. "The alteration history of late Proterozoic Wooltana volcanics, Mount Painter Province, S.A. /." Adelaide, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbs656.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology, 1992.
National grid reference SH54 - 6737-2. One coloured folded map in pocket inside back pocket. Includes bibliographical references.
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5

Kasolo, Pius Chilufya-Bwalya. "Fluid-channelling and gold mineralization within the Late Proterozoic Mwembeshi Shear Zone,Zambia." Thesis, University of Southampton, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.315515.

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6

Poole, S. "The Late Proterozoic orogenic igneous activity of the Kadaweb area, Red Sea Hills, Sudan." Thesis, University of Portsmouth, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.370180.

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7

Hapugoda, Hapugoda Udage Sarath. "Late Archaean and Early Proterozoic crustal evolution of the Georgetown Block, Northeast Queensland, Australia /." St. Lucia, Qld, 2002. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe16503.pdf.

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8

Andreasen, Kyle C. "Does the Southern Farmington Canyon Complex Record a late Archean/Early Proterozoic Accretionary Complex?" DigitalCommons@USU, 2007. https://digitalcommons.usu.edu/etd/6753.

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The Farmington Canyon Complex, situated along the Wasatch front in northern Utah, has been the target for many studies. The FCC has been interpreted to be a passive margin sedimentary wedge. Previous studies have yielded isotopic ages that broadly support an Archean age of formation, and a prominent mid-proterozoic amphibolite grade metamorphic event. Based on this study, a new interpretation for the FCC is presented. Field relations and whole-rock geochemistry as well as recent advances in understanding Archean crustal processes have resulted in the FCC to be considered as an accretionary complex that formed along the SW margin of the Wyoming province in the early Archean. Rock assemblages such as mafic and ultramafic metavolcanics have chemistries that resemble oceanic crust and arc related volcanics. The extensive quartzo-felspathic gneiss and schist units have compositions that reflect greywacke, and are presented here as a melange matrix. The quartzites have chemistries, which may represent cherts or silicified microbial mats. The field relations and timing of these rocks indicate that the FCC may represent a continental arc synchronous with the closing of an ocean basin, forming an accretionary wedge. This culminated with the mid-proterozoic metamorphic event as this continental arc collided with the Santaquin arc, as well as the SW margin of Laurentia. This amphibolite grade metamorphic event has subsequently reset or overprinted isotopic evidence and obscured any textures that may have existed. Although much has yet to be learned about Archean processes, comparison to other recognized Archean accretionary complexes has yielded striking similarities, and it is presented here that the FCC represents an active margin, and is likely an accretionary melange.
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Valentino, David W. "Tectonics of the lower Susquehhanna River region, southeastern Pennsylvania and northern Maryland: late proterozoic rifting to late paleozoic dextral transpression." Diss., Virginia Tech, 1993. http://hdl.handle.net/10919/30108.

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Pimentel, Marcio Martins. "Late Proterozoic crustal evolution of the Tocantins Province in central Brazil : an isotopic and geochemical study." Thesis, University of Oxford, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.280038.

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Книги з теми "Late Proterozoic"

1

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

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2

N. V. B. S. Dutt. Geology and mineral resources of Andhra Pradesh and late Proterozoic stratigraphy and middle and late Proterozoic tectonic evolution of peninsular India. 3rd ed. Hyderabad, India: Natural Resources Development Cooperative Society, 1986.

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3

Zang, Wen Long. Late Proterozoic and Cambrian microfossils and biostratigraphy, Amadeus Basin, central Australia. Brisbane: Association of the Australasian Palaeontologists, 1992.

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4

Allison, Carol Wagner. Paleontology of late Proterozoic and early Cambrian rocks of east-central Alaska. Washington: U.S. G.P.O., 1988.

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Allison, Carol Wagner. Paleontology of late Proterozoic and early Cambrian rocks of east-central Alaska. Washington, DC: Dept. of the Interior, 1988.

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6

Canada, Geological Survey of. The Ice Brook Formation and post-Rapitan, Late Proterozoic glaciation, Mackenzie Mountains, Northwest Territories. [s.l: s.n.], 1991.

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7

Stephen, Poole. The late proterozoic orogenic igneous activity of the Kadaweb area, Red Sea Hills, Sudan. Portsmouth: Portsmouth Polytechnic, Dept. of Geology, 1985.

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8

Aitken, J. D. The Ice Brook Formation and post-Rapitan, Late Proterozoic glaciation, Mackenzie Mountains, Northwest Territories. [Ottawa]: Energy, Mines and Resources Canada, 1991.

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9

Kukla, Peter A. Tectonics and sedimentation of a Late Proterozoic Damaran convergent continental margin, Khomas Hochland, Central Namibia. Edited by Galloway Clare Kennedy. Windhoek, Namibia: Ministry of Mines and Energy, Geological Survey of Namibia, 1992.

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10

Harlan, Stephen S. Paleomagnetic and ⁴⁰Ar/³⁹Ar geochronologic data from Late Proterozoic mafic dikes and sills, Montana and Wyoming. Washington: U.S. G.P.O., 1997.

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Частини книг з теми "Late Proterozoic"

1

Xueguang, Huang. "Mid-Late Proterozoic (Pre-Sinian) Crust." In Precambrian Crustal Evolution of China, 161–262. Berlin, Heidelberg: Springer Berlin Heidelberg, 1998. http://dx.doi.org/10.1007/978-3-662-03697-6_4.

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2

Elston, Donald P. "Middle and Late Proterozoic Grand Canyon Supergroup, Arizona." In Geology of Grand Canyon, Northern Arizona (with Colorado River Guides): Lee Ferry to Pierce Ferry, Arizona, 94–105. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft115p0094.

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3

Donnadieu, Yannick, Gilles Ramstein, Yves Goddéris, and FréDéric Fluteau. "Global Tectonic Setting and Climate of the Late Neoproterozoic: A Climate-Geochemical Coupled Study." In The Extreme Proterozoic: Geology, Geochemistry, and Climate, 79–89. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/146gm08.

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Jenkins, Gregory S. "High Obliquity as an Alternative Hypothesis to Early and Late Proterozoic Extreme Climate Conditions." In The Extreme Proterozoic: Geology, Geochemistry, and Climate, 183–92. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/146gm14.

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McMenamin, Mark A. S. "Climate, Paleoecology and Abrupt Change During the Late Proterozoic: A Consideration of Causes and Effects." In The Extreme Proterozoic: Geology, Geochemistry, and Climate, 215–29. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/146gm17.

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Åhäll, K. I., and J. S. Daly. "Late Presveconorwegian Magmatism in the Östfold-Marstrand Belt, Bohuslän, SW Sweden." In The Deep Proterozoic Crust in the North Atlantic Provinces, 359–67. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_22.

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Manby, G. M., and M. J. Hambrey. "The structural setting of the Late Proterozoic tillites of East Greenland." In The Caledonide Geology of Scandinavia, 299–312. Dordrecht: Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2549-6_25.

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Neubauer, F. "Late Proterozoic and Early Paleozoic Tectonothermal Evolution of the Eastern Alps." In The West African Orogens and Circum-Atlantic Correlatives, 307–14. Berlin, Heidelberg: Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-84153-8_13.

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Falkum, T. "Geotectonic Evolution of Southern Scandinavia in Light of a Late-Proterozoic Plate-Collision." In The Deep Proterozoic Crust in the North Atlantic Provinces, 309–22. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_18.

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10

Verschure, R. H. "Geochronological Framework for the Late-Proterozoic Evolution of the Baltic Shield in South Scandinavia." In The Deep Proterozoic Crust in the North Atlantic Provinces, 381–410. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_24.

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Тези доповідей конференцій з теми "Late Proterozoic"

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McDannell, Kalin, Daniel Holm, David A. Schneider, L. Gordon Medaris, Klaus J. Schulz, Brad S. Singer, and Brian R. Jicha. "40AR/39AR K-FELDSPAR THERMOCHRONOLOGY RESULTS FROM THE SOUTHERN LAKE SUPERIOR REGION: REHEATING AND STABILIZATION OF PROTEROZOIC LITHOSPHERE RELATED TO LATE PROTEROZOIC MAGMATIC UNDERPLATING." In 54th Annual GSA North-Central Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020nc-347712.

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2

M.E. Van den Berg, Martine, Anton Koopman, and Karen Romine and Jon Teasdale. "Evolution of the Oman Salt Basins during Late Proterozoic-Cambrian transpressional tectonics." In GEO 2008. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.246.357.

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3

Cantine, Marjorie, A. D. Rooney, Andrew H. Knoll, and Kristin Bergmann. "DEPOSITIONAL RATES IN THE EDIACARAN NAFUN GROUP, OMAN, AND THE WIDER LATE PROTEROZOIC WORLD." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-352451.

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4

Cantine, Marjorie D., Alan Rooney, Kristin Bergmann, and Andy Knoll. "Depositional rates in the Ediacaran Nafun Group, Oman, and the wider late Proterozoic world." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.5988.

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5

Adams, Donald C., Mark A. Ouimette, and Fred Moreno. "Middle-late Proterozoic extension in the Carlsbad region of southeastern New Mexico and west Texas." In 44th Annual Fall Field Conference. New Mexico Geological Society, 1993. http://dx.doi.org/10.56577/ffc-44.137.

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6

Stanevich, A. M., D. P. Gladkochub, A. M. Mazukabzov, A. G. Vakhromeev, A. V. Pospeev, T. V. Donskaya, and S. G. Babina. "Southern Baikal Region as a Model Site for Studying Late Proterozoic Deposition and Oil Generation History." In GeoBaikal 2018. Netherlands: EAGE Publications BV, 2018. http://dx.doi.org/10.3997/2214-4609.201802016.

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7

Zylstra, Scott, Nicholas J. Van Buer, Nicholas J. Van Buer, Jonathan A. Nourse, Jonathan A. Nourse, Karissa Vermillion, and Karissa Vermillion. "LATE CRETACEOUS PLUTONIC AND METAMORPHIC OVERPRINT OF PROTEROZOIC METASEDIMENTS OF ONTARIO RIDGE, EASTERN SAN GABRIEL MOUNTAINS, CA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-305768.

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8

Conrey, Richard M., David G. Bailey, Drew Castronovo, Martin J. Streck, and Jared W. Singer. "LATE MIOCENE XENOCRYST-BEARING LAVAS ON GREEN RIDGE, CENTRAL OREGON CASCADE RANGE: IMPLICATIONS FOR THE FORMATION OF PROTEROZOIC MASSIF ANORTHOSITE." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-358028.

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9

Ghoshmaulik, Sangbaran, Sourendra Kumar Bhattacharya, Anindya Sarkar, and Pallab Roy. "Triple Oxygen Isotope Clue of Enigmatic Nodular Chert Formation in Vindhyan Carbonates and an Insight into the Late Neo-Proterozoic Seawater Composition." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.822.

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10

Sarolta, Lőrincz, Melinte-Dobrinescu Mihaela, Relu Roban, Mihai Ducea, Valentina Cetean, Marian Munteanu, and Vlad-Victor Ene. "Magmatic clasts from turbidites in the Moldavide nappes as indication of a late Proterozoic subduction event in the foreland of the Eastern Carpathians." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10869.

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Звіти організацій з теми "Late Proterozoic"

1

Trettin, H. P. Chapter 9: the Proterozoic To Late Silurian Record of Pearya. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/100311.

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2

Aitken, J. D. The Ice Brook Formation and post-Rapitan, late Proterozoic glaciation, Mackenzie Mountains, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132664.

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3

Teitz, M., and E. W. Mountjoy. The Yellowhead and Astoria carbonate platforms in the late proterozoic upper miette group, Jasper, Alberta. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120182.

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4

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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5

Pe-Piper, G. Geochemistry of late Proterozoic plutonic rocks from Flemish Cap, east of the Grand Banks of Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1992. http://dx.doi.org/10.4095/132878.

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6

Castonguay, S., D. Lavoie, and N. Pinet. The Lower Paleozoic Humber zone in eastern Canada (latest Proterozoic (Ediacaran) to Late Ordovician) - Geological framework. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2009. http://dx.doi.org/10.4095/226320.

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7

Stewart, W. D. Late Proterozoic to early tertiary stratigraphy of Somerset Island and northern Boothia Peninsula, District of Franklin, N.W.T. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122372.

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8

Lavoie, D., N. Pinet, and S. Castonguay. The Lower Paleozoic Humber zone in eastern Canada (latest Proterozoic (Ediacaran) to Late Ordovician) - Hydrocarbon system data. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2009. http://dx.doi.org/10.4095/226321.

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9

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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10

Sweetkind, D. S., and D. K. White. Facies analysis of Late Proterozoic through Lower Cambrian rocks of the Death Valley regional ground-water system and surrounding areas, Nevada and California. Office of Scientific and Technical Information (OSTI), March 2002. http://dx.doi.org/10.2172/793126.

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