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|Statement||F. Cook and P. Erdmer, compilers.|
|Series||Lithoprobe report -- no. 69|
|Contributions||Cook, Frederick A., Erdmer, Philippe, 1956-, Cordilleran Tectonics Workshop (1999 : Calgary, University of Calgary)|
|The Physical Object|
|Pagination||340 p. :|
|Number of Pages||340|
Download Lithoprobe Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) and Cordilleran Tectonics Workshop
The North American Cordillera in Canada and Alaska has been investigated through coincident and coordinated geological, geochemical, and geophysical studies along three corridors: (1) the Lithoprobe Southern Cordillera transect, (2) the ACCRETE and Lithoprobe Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) transects, and (3) the Trans-Alaska Crustal.
Reflection patterns along Lithoprobe Slave – Northern Cordillera Lithospheric Evolution (SNORCLE) seismic reflection line 1 in the southwestern Slave Province are interpreted asCited by: How is Slave Northern Cordillera Lithosphere Evolution Project abbreviated.
SNORCLE stands for Slave Northern Cordillera Lithosphere Evolution Project. SNORCLE is defined as Slave Northern Cordillera Lithosphere Evolution Project very rarely.
Lithoprobe is Canada's national, collaborative, multidisciplinary, Earth science research project established to develop a comprehensive understanding of the evolution of.
A children’s book, based on LITHOPROBE results, that is intended for mid-grade students (ages ) was authored by John Wilson (Fig. Noting the value of such a book for educational purposes, LITHOPROBE contracted the preparation of Teachers’ Companion Material, to encourage use of the children’s book in the educational system.
The Southern Canadian Cordillera Transect of Lithoprobe: Introduction Article (PDF Available) in Canadian Journal of Earth Sciences 32(10) February with 52 ReadsAuthor: Frederick Cook.
Lithoprobe deep seismic reflection data from the northwestern Canadian Shield provide images of structures to the base of the lithosphere between the Archean Slave. understanding of the evolution of the northern North American continent. With rocks representing 4 b.y.
of Earth history, the Canadian landmass and off-shore margins provide an exceptional opportunity to gain new perspectives on continental evolution.
Lithoprobe’s 10 study areas span the country and geological time. A pan-Lithoprobe syn. Ancient crystalline basement in western Canada: its influence on the platformal sedimentary cover, and basement remnants across the Cordillera; in: F.
Cook and P. Erdmer (comps.), Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop Meeting, University of Calgary; Lithoprobe Report # 72, p.
In: Cook FA, Erdmer P (eds) Lithoprobe Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) and Cordilleran Tectonics Workshop, Lithoprobe rep pp 76–80 Google Scholar Ross GM, Villeneuve ME, Theriault RJ () Isotopic provenance of the lower Muskwa assemblage (Mesoproterozoic, Rocky Mountains, British Columbia): new clues to Cited by: The current understanding of the structure and geological history of the crust in the study area is based on regional LITHOPROBE geophysical transects, such as Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) and Alberta Basement Transect (ABT), integrated with geological and geochronological studies (e.g.
Ross et al. ; Pilkington Cited by: Mid-crustal channel flow in large hot orogens: results from coupled thermal-mechanical models, in: Cook, F., and Erdmer, P., Slave Northern Cordillera Lithospheric Evolution (SNORCLE) and Cordilleran Tectonics Workshop, Lithoprobe Report, 79, Hyndman RD, Flück P, Mazzotti S, Lewis TJ, Ristau J, Leonard L () The lithoprobe slave-northern cordillera lithospheric evolution (SNORCLE) transect/current tectonics of the northern Canadian Cordillera; La géotraverse de l’évolution lithosphérique de la Cordillère du Nord et de la province du lac des Esclaves (SNORCLE).Author: J.
Cassidy, H. Kao, John Ristau, A. Bent. In Slave–Northern Cordillera Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop. Edited by F. Cook and P. Erdmer.
Lithoprobe Report Cited by: 6. Edwards, BR, Kopylova, ML, Russell, JK () Petrology of the Lithosphere beneath the Northern Cordillera. In Cook, F.
and Erdmer, P. (compilers), Slave-northern Cordilleran Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop Meeting (March ), University of Calgary, Lithoprobe Report No. 56, Approximately $, is available for geoscientific projects which complement the existing and planned seismic and electromagnetic programs and contribute in a significant way to the scientific objectives of the Slave-Northern Cordillera Lithospheric Evolution and Western Superior Transects or assist Pan-Lithoprobe synthesis, and for projects.
COOK,F and ERDMER,P (editors) () Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop. Lithoprobe Rep University of Calgary, pp. Tectonics of northwestern North America. D'LEMOS,RS, STRACHAN,RA and TOPLEY,CG (editors) () The Cadomian Orogeny.
Lower Eocene fluvial strata in the Chuckanut Formation preserve abundant bird and mammal tracks. Reptile trace fossils include footprints from a small turtle (ichnogenus Chelonipus), and several Crocodylian trackways that consist of irregularly spaced footprints associated with linear tail drag marks.
The latter trackways represent “punting” locomotion, where a Cited by: 1. Cook, P. Erdmer (Eds.), Slave-northern Cordillera Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop Meeting (February ), 72, University of Calgary, Lithoprobe Report (), pp.
Cited by: 1. In: (edited by Cook, F. & Erdmer, P.) Slave-Northern Cordillera Lithospheric Evolution (SNORCLE) Transect and Cordilleran Tectonics Workshop Meeting (March ), University of Calgary Lithoprobe Rep Mezger, J. (): The Kluane Metamorphic Assemblage, SW Yukon - an accretionary wedge of backarc basin affinity Limnogeology: tales of an evolving Earth - 4th Limnogeology Congress Barcelona, July- Programme with abstracts book, Mezger, J.
(): Differential staurolite rotation dependent on pre-deformational length axis orientation.- Reading the rocks: textures and timings on all scales in metamorphism. Mezger, J. E., Schnapperelle, S.
& Rölke, C. (in press): Evolution of the Central Pyrenean Mérens fault controlled by near collision of two gneiss domes. - Hallesches Jahrbuch für Geowissenschaften. Mezger, J. (): Rotation of irregular staurolite porphyroblasts in a simple shear dominated shear zone controlled by initial growth.
The Upper Hazelton Group and its significance for the Jurassic evolution of the Stikine terrane, British Columbia. Cordilleran tectonics workshop, Geological Association of. Abstract Mid-Cretaceous strata within the Tintina Trench, 3 km west of the community of Ross River, contain evidence of deposition in two distinct, alternating, fluvial settings.
Coal-bearing, mud-dominated strata are commonly associated with high-constructive sandy channel systems, with extensive overbank, levee and splay deposits. Channels are between 3 and 30 m wide.
Abstract The 20‐ to ‐m‐thick > Ga Bell Lake group is a siliciclastic‐dominated succession in the Slave craton that contains features consistent with continental rifting.
The Archean succession is composed of four principal lithofacies: (1) conglomerate, (2) quartz arenite, (3) sandstone‐argillite, and (4) argillite‐ by: Mehmet F. Taner, Robert A. Gault, and T. Scott Ercit VANADIUM MINERALIZATION AND ITS INDUSTRY IN CANADA VANADIUM MINERALIZATION AND ITS INDUSTRY IN CANADAVANADIUM MINERALIZATION AND ITS INDUSTRY.
B Fullerton, pp. 81â 83 Color profile: Disabled Composite Default screen Lower Paleozoic stratigraphic and biostratigraphic correlations in the Canadian Cordillera: implications for the tectonic evolution of the Laurentian margin1 Leanne J.
Pyle and Christopher R. Barnes. The Yellowknife greenstone belt has produced approximately 14 million ounces of gold, 13 of which came from the well explored southern half of the belt. The northern half of the belt, where the Discovery Property (1 million ounce past producer) is located, is not as well explored, but geologically very similar to the gold producing southern half.
Gold on the Discovery Property, Author: William H. Whitty. This thesis investigates glaciovolcanism in the Mount Cayley volcanic field (MCVF) of southwestern British Columbia's Garibaldi Volcanic Belt (GVB). The MCVF is dominated by intermediate magma compositions, has been intermittently glaciated, and has extreme topography.
No study to date has focused on intermediate composition glaciovolcanic deposits Cited by: 4. Transcript. 1 Citations Acknowledging using our IRIS-Related facilities and Data as of Decemberupdated December Please send corrections and/or additions to [email protected]. 2 Aagaard, B.T., R.W.
Graves, A. Rodgers, T.M. Brocher, R.W. Simpson, D. Dreger, N. Petersson, S.C. Larsen, S. Ma, and R.C. Jachens (), 'Ground-Motion modeling of. Precambrian crust and lithosphere beneath the Northern Canadian Cordillera discovered by LITHOPROBE seismic reflection profiling.
NASA Astrophysics Data System (ADS) Clowes, R. Citations. Acknowledging or using IRIS-Related facilities and Data. As of August Please send corrections and/or additions to [email protected] Abbott, R.E. (), "Geophysical constraints on seismic hazard and tectonics in the western Basin and Range".Thesis in Geophysics, Department of Geological Sciences, Reno: University of Nevada, Reno.
Abbott. O Scribd é o maior site social de leitura e publicação do mundo.5/5(1). OFR - Free download as PDF File .pdf), Text File .txt) or read online for free. Bimodal tholeiitic-dacitic magmatism and the Early Precambrian crust. USGS Publications Warehouse. Barker, F.; Peterman, Z.E.
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