Bibliografías temáticas / Plutonic suite

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Literatura académica sobre el tema "Plutonic suite"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 1 de febrero de 2022

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Artículos de revistas sobre el tema "Plutonic suite"

1

Davis, W. J., and Wouter Bleeker. "Timing of plutonism, deformation, and metamorphism in the Yellowknife Domain, Slave Province, Canada." Canadian Journal of Earth Sciences 36, no. 7 (1999): 1169–87. http://dx.doi.org/10.1139/e99-011.

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U-Pb zircon, titanite, and monazite ages for plutonic rocks are used to constrain the timing of post-2660 Ma deformational and metamorphic events in the Yellowknife Domain, southern Slave Province. Diorite and tonalite plutons of the Defeat Suite yield ages of 2628 ± 3 and 2624 ± 3 Ma, older than previous, less precise estimates for this suite of ca. 2618-2620 Ma. The Defeat Suite plutons crosscut and postdate upright F1 folds in turbidites of the ca. 2680-2660 Ma Burwash Formation. D1 deformation is therefore bracketed between 2660 and 2630 Ma. The D1 event significantly predates deposition o
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2

Greig, C. J., R. L. Armstrong, J. E. Harakal, D. Runkle, and P. van der Heyden. "Geochronometry of the Eagle Plutonic Complex and the Coquihalla area, southwestern British Columbia." Canadian Journal of Earth Sciences 29, no. 4 (1992): 812–29. http://dx.doi.org/10.1139/e92-068.

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New U–Pb, K–Ar, and Rb–Sr dates from the Eagle Plutonic Complex and adjacent map units place timing constraints on intrusive and deformational events along the southwestern margin of the Intermontane Belt. U–Pb zircon minimum dates for Eagle tonalite and gneiss (148 ± 6, 156 ± 4, and 157 ± 4 Ma) document previously unrecognized Middle to Late Jurassic magmatism and syn-intrusive deformation along the eastern margin of the Eagle Plutonic Complex and the southwestern margin of the Intermontane terrane. Widespread mid-Cretaceous (Albian–Cenomanian) resetting of K–Ar and Rb–Sr isotopic systematics
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3

Bédard, L. Paul, and John N. Ludden. "Nd-isotope evolution of Archaean plutonic rocks in southeastern Superior Province." Canadian Journal of Earth Sciences 34, no. 3 (1997): 286–98. http://dx.doi.org/10.1139/e17-026.

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The Opatica plutonic belt, Abitibi greenstone belt, and Pontiac Subprovince represent a major proportion of the southeastern Superior Province, which was formed and accreted rapidly between approximately 2.9 and 2.8 Ga. Plutons in these belts are grouped into four types: (i) trondhjemite–tonalite–granodiorite (TTG) suite (2.82–2.69 Ga), (ii) monzodiorite (MZD) suite (2.697–2.669 Ga), (iii) late alkaline granitoid (ALK) suite (2.68–2.67 Ga), and (iv) anatectic granite and monzonite (ANA) suite (2.69–2.64 Ga). The four suites are represented in all belts and show similar petrography and geochemi
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4

Azadbakht, Zeinab, Christopher E. M. McFarlane, and David R. Lentz. "Precise U-Pb ages for the cogenetic alkaline Mount LaTour and peraluminous Mount Elizabeth granites of the South Nepisiguit River Plutonic Suite, northern New Brunswick, Canada." Atlantic Geology 52 (October 24, 2016): 189. http://dx.doi.org/10.4138/atlgeol.2016.009.

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The South Nepisiguit River Plutonic Suite consists of various phases of felsic to mafic plutonic rocks of early Devonian age in northern New Brunswick. The felsic portion of this intrusive suite includes a large pluton of homogeneous, peraluminous biotite granite (the Mount Elizabeth Granite), which is flanked on its western side by the alkaline Mount LaTour Granite. New in situ and mineral separate U-Pb Laser Ablation-Inductively Coupled Plasma Mass Spectro-metry analyses of monazite and zircon grains from both sides of the suite define a crystallization age of 417.3 ± 0.96 Ma for the Mount E
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Puchalski, Raya C., Sandra M. Barr, and Chris E. White. "Field relations and petrology of the Trafalgar Plutonic Suite and comparisons with other Devonian granitoid plutons in the Meguma terrane, Nova Scotia, Canada." Atlantic Geology 56 (April 18, 2020): 001–17. http://dx.doi.org/10.4138/atlgeol.2020.001.

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The Trafalgar Plutonic Suite intruded metasedimentary rocks of the Goldenville and Halifax groups in the northeastern part of the Meguma terrane of southern Nova Scotia at about 374 Ma, based on previously published U–Pb and 40Ar/39Ar mineral ages. Using field and petrographic observations, the suite is divided into 20 different plutons on the combined basis of variations in grain size (fine, medium, or coarse), texture (equigranular or porphyritic) and modal mineralogy (quartz diorite/tonalite, granodiorite, monzogranite, and syenogranite). The granodiorite, monzogranite, and syenogranite plu
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6

Lindline, Jennifer, William A. Crawford, and Maria Luisa Crawford. "A bimodal volcanic–plutonic system: the Zarembo Island extrusive suite and the Burnett Inlet intrusive complex." Canadian Journal of Earth Sciences 41, no. 4 (2004): 355–75. http://dx.doi.org/10.1139/e04-009.

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The Zarembo Island volcanic rocks and the Burnett Inlet plutonic complex in central southeastern Alaska were investigated to determine if they are genetically related. The Zarembo Island volcanic suite consists of basalt, andesite, and rhyolite lava flows, which exhibit features that suggest simultaneous eruptions of mafic and felsic lavas. Five kilometres to the southeast, the broadly layered Burnett Inlet plutonic complex consists of gabbro–diorite and granite plutons that also show characteristics of contemporaneous mafic and felsic magmatism. These bimodal volcanic and plutonic rocks are s
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Ketchum, John WF, Sandra M. Barr, Nicholas G. Culshaw, and Chris E. White. "U-Pb ages of granitoid rocks in the northwestern Makkovik Province, Labrador: evidence for 175 million years of episodic synorogenic and postorogenic plutonism." Canadian Journal of Earth Sciences 38, no. 3 (2001): 359–72. http://dx.doi.org/10.1139/e00-085.

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New U–Pb zircon, titanite, and monazite ages reported here, along with existing age data, demonstrate that granitoid bodies in the northwestern segment of the Paleoproterozoic Makkovik Province, Labrador, are of three distinct ages. The redefined Island Harbour Bay plutonic suite consists of varied dioritic to granitic units that were syntectonically emplaced into Archean crust of the Kaipokok domain between ca. 1895 Ma and 1870 ± 2 Ma. This plutonism occurred during the early stages of the Makkovikian Orogeny in an obliquely convergent, Andean continental margin setting. The Hares Islands and
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Symons, D. T. A., K. Kawasaki, C. J. R. Hart, and M. J. Harris. "A paleomagnetic test for northward tectonic transport of the eastern Selwyn Basin, northern Canadian Cordillera: data from the mid-Cretaceous Ragged Pluton." Canadian Journal of Earth Sciences 45, no. 7 (2008): 860–69. http://dx.doi.org/10.1139/e08-028.

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Ragged Pluton is a member of the Tungsten Plutonic Suite in the eastern Selwyn Basin. This circular massive 97 Ma granitic pluton is ∼5 km in diameter. It intrudes deformed and metamorphosed clastic strata of the Neoproterozoic to Lower Cambrian Vampire Formation. Thermal and alternating field step demagnetization data for 216 specimens from 21 plutonic sites isolated a stable characteristic remanent magnetization (ChRM) direction at 20 sites of declination D = 325.9°, inclination I = 80.4° (α95 = 2.7°, k = 142). Thermal demagnetization and saturation remanence analysis show that the ChRM is c
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9

Cui, Yao, and J. K. Russell. "Magmatic origins of calc-alkaline intrusions from the Coast Plutonic Complex, southwestern British Columbia." Canadian Journal of Earth Sciences 32, no. 10 (1995): 1643–67. http://dx.doi.org/10.1139/e95-131.

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Major element, trace element, and rare earth element data are presented for Permian to Tertiary calc-alkaline plutonic and volcanic rocks along a transect across the southern Coast Plutonic Complex from Vancouver to Anderson Lake. Late Jurassic to Late Cretaceous plutons are divided into two compositional suites based on mineralogy: (1) the hornblende intrusive suite (tonalite, quartz diorite, diorite, and gabbro) characterized by abundant modal hornblende and little or no K-feldspar, and (2) the K-feldspar intrusive suite (mainly granite and granodiorite) containing significant modal K-feldsp
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Selby, David, Robert A. Creaser, and Bruce E. Nesbitt. "Major and trace element compositions and Sr-Nd-Pb systematics of crystalline rocks from the Dawson Range, Yukon, Canada." Canadian Journal of Earth Sciences 36, no. 9 (1999): 1463–81. http://dx.doi.org/10.1139/e99-058.

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Geochemical (major, trace, and rare earth elements) and isotopic (Nd, Sr, and Pb) data of the Devono-Mississippian Wolverine Creek Metamorphic Suite, mid-Cretaceous Dawson Range batholith, mid-Cretaceous Casino Plutonic Suite, and Late Cretaceous plutons provide new information on the origin and evolution of the rocks from the Dawson Range in west-central Yukon, northern Canadian Cordillera. Isotopic and other geochemical data for the Wolverine Creek Metamorphic Suite metasedimentary rocks indicate that the detrital components were derived from two distinct provenances: (1) the North America c
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Tesis sobre el tema "Plutonic suite"

1

Tice, Peter. "Petrology and Geochemical Evolution of the East Hill Suite of the Mont Saint-Hilaire Alkaline Plutonic Complex." ScholarWorks@UNO, 2010. http://scholarworks.uno.edu/td/1229.

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The Mont Saint-Hilaire alkaline complex, Québec, is a Cretaceous rift-related intrusion comprising two gabbroic suites and the East Hill suite, an assemblage of several distinct nepheline syenites and evolved syenitic rocks. Whole-rock analysis of the East Hill suite reveals two fractionation trends, one which is described by the syenitic lithologies and one by the evolved syenites and syenoids. A lamprophyric unit stands on its own, geochemically, consistent with typical lamprophyre petrogenesis. Whole-rock geochemistry of the East Hill suite shows moderate silica content but highly alkaline
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2

Dwyer, Berni Lori. "A compiled geological, geochemical, and metallogenic study of a magmatic nickel-copper sulphide occurrence at the Cirque property, Nain Plutonic suite, Northern Labrador /." Internet access available to MUN users only, 2001. http://collections.mun.ca/u?/theses,36819.

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Tice, Peter. "Mineralogy of Eudialyte Group Minerals From the East Hill Suite Of the Mont Saint-Hilaire Alkaline Plutonic Complex, Including an Alternative Site-Assignment Algorithm & A Proposed Classification System." ScholarWorks@UNO, 2009. http://scholarworks.uno.edu/td/965.

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The twenty approved members of the eudialyte group are complex zirconosilicates, primarily with general formula N15M(1)6M(2)3M(3)M(4)Z3[Si24O72]O4X2. An algorithm was created to address the inherent recalculation difficulties in the absence of single-crystal X-ray data and was an overall improvement over previous schemes. Eudialyte group minerals were analyzed from the East Hill Suite of the Mont Saint-Hilaire alkaline complex. Recalculations revealed previously undocumented eudialyte-group compositions and degrees of chemical zonation. These data suggest that late-stage melt heterogenei
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Dias, Luiz Gustavo da Silveira. "Caracteriza??o geol?gica, geoqu?mica e geocronol?gica da su?te plut?nica enoproteroz?ica da regi?o de Serrinha, por??o centro-leste do maci?o S?o Jos? de Campestre, sudeste do RN." Universidade Federal do Rio Grande do Norte, 2006. http://repositorio.ufrn.br:8080/jspui/handle/123456789/18839.

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Made available in DSpace on 2015-03-13T17:08:39Z (GMT). No. of bitstreams: 1 LuizGSD_ate_cap6.pdf: 3498562 bytes, checksum: 2d2d95d878c0320cd578c1fd98d02cfe (MD5) Previous issue date: 2006-08-31<br>Coordena??o de Aperfei?oamento de Pessoal de N?vel Superior<br>The of Serrinha plutonic suite, northeastern portion of the Borborema Province (NE Brazil), is characterized by a voluminous and diversified magmatism of Neoproterozoic age, intrusive in the Archean to Paleoproterozoic gneissic-migmatitic basement of the S?o Jos? de Campestre massif. Field relations and petrographic and geochemical
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Wilson, Sharmoney. "The petrogenesis of the intermediate to mafic rocks of the yzerfontein subsuite, and their relationship to-, and paragenesis of hydrothermal veining, cape granite suite, saldania belt, south africa." University of Western Cape, 2020. http://hdl.handle.net/11394/7398.

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>Magister Scientiae - MSc<br>The 535 Ma post-orogenic Yzerfontein Pluton is a composite pluton that comprises rocks of mafic, intermediate and felsic compositions belonging to the shoshonitic series. The Yzerfontein Pluton forms part of the Cape Granite Suite of the Late-Proterozoic to Early-Cambrian Pan-African Saldania Belt. In this study, major- and trace-element data for the various rocks of the pluton, which act as hosts to extensive hydrothermal veining, are presented and integrated with the petrographic examination of the host rocks in order to constrain their petrogenesis.
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Yarr, Timothy Roderick. "A petrological study of the appinite suite associated with the Ardara pluton, Co. Donegal, Ireland." Thesis, University of St Andrews, 1992. http://hdl.handle.net/10023/15565.

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Appinites are enigmatic rocks commonly associated with major I-type plutons in the Caledonian orogen, a number of different models have been proposed for the origin of their parental magmas and unusual textural characteristics. The appinite cluster associated with the Ardara pluton has been studied using petrological techniques with the aim of understanding these features as well as their relationships to the main pluton. The approach of this study has been to select a few appinite bodies considered to be representative of the whole Ardara appinite suite, and to study each in detail in paralle
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Ham, Natalie M. "Structural and magnetic fabric study of the late Archean Sparrow and Prosperous plutons, Prosperous suite, Slave Province, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/MQ58459.pdf.

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Henney, Paul J. "The geochemistry and petrogenesis of the minor intrusive suite associated with the late Caledonian Criffell-Dalbeattie pluton, SW Scotland." Thesis, Aston University, 1991. http://publications.aston.ac.uk/14390/.

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The Criffell-Dalbeattie pluton from SW Scotland is one of a suite of late Caledonian granitoids which are associated with extensive, contemporaneous and compositionally diverse suits of minor intrusions. The minor intrusive suite associated with the Criffell-Dalbeattie pluton is dominantly composed of a series of porphyritic microdiorites, microgranodiorites and microgranites known collectively as the porphyrite-porphyry series. This series can be divided into two groups, the porphyrites and the quartz porphyries, on the basis of petrography and geochemistry although there is some compositiona
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ROSA, SEIXAS LUIS ANTONIO. "Petrologie de la suite ttg de la bordure nord du batholite d'alto maranhao et du pluton congonhas, minas gerais, bresil." Paris 11, 2000. http://www.theses.fr/2000PA112075.

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Cette etude presente des donnees de terrain, mineralogiques et geochimiques de deux massifs plutoniques mis en place a 2. 1 - 2. 2 ga au debut de l'orogenese transamazonienne dans la portion meridionale du craton do sao francisco, minas gerais, bresil. Ce magmatisme se caracterise par une suite de roches tonalitiques, granodioritiques et trondhjemitiques du type ttg haut al - adakitique, issue d'une source juvenile et probablement associee avec subduction. Il met en evidence differentes contributions des sources de magmas (croute vs. Manteau) et differents processus dans les chambres magmatiqu
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10

Hogan, John Patrick. "Mineralogical, chemical and isotopic diversity in plutonic rock suites from the Coastal Maine Magmatic Province:the role of source region heterogeneity, tectonic setting and magmatic processes." Diss., Virginia Tech, 1990. http://hdl.handle.net/10919/39074.

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This dissertation represents an investigation of the mid-Paleozoic tectono-thermal and kinematic evolution of the crust in eastern coastal Maine as recorded by the plutonic rocks of this region. The first chapter describes the plutonic rocks of the Coastal Maine Magmatic Province. A tectonic model is developed in which late Ordovician-Silurian bimodal magmatism is interpreted to reflect crustal melting as a result of intraplating of mantle melts at high crustal levels during a period of tension. Large scale melting of lower crustal source regions, represented by voluminous intrusion of Devoni
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Libros sobre el tema "Plutonic suite"

1

Ford, Arthur B. The Sitkoh Bay alkalic plutonic suite: Silurian or older alkalic magmatism on eastern Chichagof Island, southeastern Alaska. U.S. Dept. of the Interior, Geological Survey, 1990.

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Gable, Dolores J. Tabulation of modal and chemical analyses for Silver Plume Quartz Monzonite (Silver Plume Granite), Berthoud Plutonic Suite, Front Range, Colorado. U.S. Dept. of the Interior, Geological Survey, 1985.

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Gable, Dolores J. Tabulation of modal and chemical analyses for Silver Plume Quartz Monzonite (Silver Plume Granite), Berthoud Plutonic Suite, Front Range, Colorado. U.S. Dept. of the Interior, Geological Survey, 1985.

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Henney, Paul James. The geochemistry and petrogenesis of the minor intrusive suite associated with the late Caledonian Criffell-Dalbeattie pluton, SW Scotland. Aston University. Department of Geological Science, 1991.

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Sheridan, Amy W. Geochemistry of the Milford Plutonic Suite. 1988.

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Loftenius, Christer. The geochemistry and the petrogenesis of the Sharpners Pond plutonic suite, NE Massachusetts. 1988.

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The Sitkoh Bay alkalic plutonic suite: Silurian or older alkalic magmatism on eastern Chichagof Island, southeastern Alaska. U.S. Dept. of the Interior, Geological Survey, 1990.

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Tabulation of modal and chemical analyses for Silver Plume Quartz Monzonite (Silver Plume Granite), Berthoud Plutonic Suite, Front Range, Colorado. U.S. Dept. of the Interior, Geological Survey, 1985.

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Capítulos de libros sobre el tema "Plutonic suite"

1

Briqueu, L., C. Mével, and F. Boudier. "Sr, Nd and Pb Isotopic Constraints in the Genesis of a Calc-Alkaline Plutonic Suite in Oman Ophiolite Related to the Obduction Process." In Ophiolite Genesis and Evolution of the Oceanic Lithosphere. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3358-6_26.

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Lagabrielle, Yves, Daniel Bideau, Mathilde Cannat, Jeffrey A. Karson, and Catherine MéVel. "Ultramafic-Mafic Plutonic Rock Suites Exposed Along the Mid-Atlantic Ridge (10°N-30°N). Symmetrical-Asymmetrical Distribution and Implications for Seafloor Spreading Processes." In Faulting and Magmatism at Mid-Ocean Ridges. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm106p0153.

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Kumar, Naveen, and Naresh Kumar. "Petro-Mineralogical and Geochemical Study of the Acid Magmatic Rocks of Tusham Ring Complex, NW Peninsular India." In Petrology [Working Title]. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.95836.

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The present contribution reports about the field and petrographical observations which are very important to explain the magmatic evolution and geodynamic setting of Tusham Ring Complex (TRC). TRC is associated with A-type acid volcano-plutonic rock-association which is very common characteristics of Neoproterozoic Malani Igneous Suite (MIS). Based on the geological field information, the investigated rock-types are classified as volcanic phase, plutonic phase and dyke phase. Petrographically, rhyolites show porphyritic, granophyric, glomeroporphyritic, aphyritic, spherulitic and perlitic textures whereas granites show hypidomorphic, granophyric and microgranophyric textures. Based on mineral chemistry and whole-rock geochemistry, the petro-mineralogical results are justified and proposed that the rocks under study belong to A-type affinity, within-plate and anorogenic magmatism. Physiochemical features i.e. F and Cl-rich biotite, pegmatite rim, high mineralized veins, micro-granular enclaves and altered mineralogy indicate rock-fluid interactions which are caused by magmatic origin or secondary metasomatic alteration superimposed on the host rock.
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McSween, Harry Y., and Ralph P. Harvey. "Concord Plutonic Suite: Pre-Acadian gabbro-syenite intrusions in the southern Appalachians." In The Nature of Magmatism in the Appalachian Orogen. Geological Society of America, 1997. http://dx.doi.org/10.1130/0-8137-1191-6.221.

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John, Barbara E., and Joe Wooden. "Chapter 5: Petrology and geochemistry of the metaluminous to peraluminous Chemehuevi Mountains Plutonic Suite, southeastern California." In Geological Society of America Memoirs. Geological Society of America, 1990. http://dx.doi.org/10.1130/mem174-p71.

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Kumar, Naresh, and Radhika Sharma. "Petrology and Geochemistry of Nakora Ring Complex with Emphasis on Tectonics and Magmatism, Neoproterozoic Malani Igneous Suite, Western Rajasthan, India." In Volcanology [Working Title]. IntechOpen, 2021. http://dx.doi.org/10.5772/intechopen.98609.

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The present contribution reports on the field, petrographical and geochemical observations of the volcano-plutonic rocks of the Nakora Ring Complex (NRC) from the Neoproterozoic, Malani Igneous Suite (MIS) (Northwestern Peninsular India) and confers about their magmatic evolution and tectonic implications. Three magmatic phases are notable in the NRC which is Extrusive, Intrusive and Dyke phase where with small quantities of basaltic flows was initiated and accompanied by extensive/voluminous acidic flows. Petrographically, rhyolite shows flow bands, porphyritic, spherulitic, aphyritic and perlitic textures whereas basalt flows are distinguished by the presence of labradorite in lath-shaped crystals (plagioclase feldspar) and clinopyroxene (augite). The presence of high silica and total alkalis in NRC rocks, as well as high field strength elements (HFSE), enrichment of trace elements and negative anomalies of Sr., Eu, P, and Ti indicates that the emplacement of the lava flows was controlled by complex magmatic processes such as fractional crystallization, crustal contamination and partial melting. The association of basalt-trachyte-rhyolite means that the magma chamber was supplied a significant amount of heat to the crust before the eruption. Moreover, a volcanic vent was also reported at NRC where rhyolite was associated with agglomerate, volcanic breccia, perlite and tuff. The current research proposed that the Neoproterozoic magmatism at NRC was controlled by rift-related mechanism and produced from crustal source where the heat was supplied by mantle plume.
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Rapela, C. W., and R. J. Pankhurst. "Monzonite suites: the innermost Cordilleran plutonism of Patagonia." In The Third Hutton Symposium on the Origin of Granites and Related Rocks. Geological Society of America, 1996. http://dx.doi.org/10.1130/0-8137-2315-9.193.

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Kerr, Andrew. "Space-time composition relationships among Appalachian-cycle plutonic suites in Newfoundland." In The Nature of Magmatism in the Appalachian Orogen. Geological Society of America, 1997. http://dx.doi.org/10.1130/0-8137-1191-6.193.

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Actas de conferencias sobre el tema "Plutonic suite"

1

Dorais, Michael J. "THE NEW HAMPSHIRE PLUTONIC SUITE: WHAT DO WE KNOW, WHAT PROBLEMS REMAIN?" In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328324.

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Wilson, Frederic H., Susan M. Karl, and Lisa Koeneman. "SEARCHING FOR THE SAINT ELIAS PLUTONIC SUITE IN GLACIER BAY NATIONAL PARK AND PRESERVE, ALASKA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286596.

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Jacobi, Robert D., Charles Mitchell, and Charles Mitchell. "COEVAL DEVELOPMENT OF TACONIC RETRO-ARC ALLOCHTHONS, UTICA BASIN, ASH BEDS, AND THE BIMODAL OLIVERIAN PLUTONIC SUITE: EFFECTS OF ASEISMIC RIDGE SUBDUCTION?" In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310761.

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Barr, Sandra M., Brent V. Miller, and Chris E. White. "TONIAN ALKALI ANORTHOSITE, FERRONORITE, AND GABBRO IN THE LOWER COVERDALE PLUTONIC SUITE, SOUTHERN NEW BRUNSWICK, CANADA: AN AMAZONIAN PART OF GANDERIAN BASEMENT?" In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344175.

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Subba Rao, D. V., E. V. S. S. K. Babu, V. Balaram, and G. Vidyasagar. "Geochemical Study of the Ultramafic-Mafic Plutonic and Volcanic Suites of the Nuggihalli Schist Belt, Western Dharwar Craton." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63393.

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Hildebrand, Robert S., and Joseph B. Whalen. "MID-CRETACEOUS CLOSURE OF A MARGINAL SEAWAY BY WESTWARD SUBDUCTION AND MANTLE ORIGIN OF POST-COLLISIONAL SLAB FAILURE PLUTONIC SUITES IN THE NORTH AMERICAN CORDILLERA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336274.

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Uematsu, Shinichi, Noriyuki Tobita, and Toru Koakutsu. "Decommissioning of a Plutonium-Contaminated Waste Incinerator Facility (I)." In ASME 2001 8th International Conference on Radioactive Waste Management and Environmental Remediation. American Society of Mechanical Engineers, 2001. http://dx.doi.org/10.1115/icem2001-1229.

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Abstract A plutonium-contaminated waste incinerator facility (PWIF) was operated from 1983 to 1989 to demonstrate the treatment of combustible plutonium-contaminated wastes from MOX fuel production facilities in Tokai works of the former Power Reactor and Nuclear Fuel Development Corporation (PNC). PWIF has following features: 1) Silicon carbide cakes (approximately 300kg) were filled in the incinerator. 2) The incinerator had the multi-layer structure, and the plutonium-contaminated ashes adhered on the inner surface of the incinerator. 3) The space for dismantling was not maintained sufficie
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Scheland, Cullen L., Vali Memeti, Vali Memeti, et al. "SHIFT FROM SOURCE TO SYSTEM CONTROL ON PLUTON COMPOSITIONS RECORDED IN THE MIGRATED JACK MAIN CANYON INTRUSIVE SUITE IN THE CENTRAL SIERRA NEVADA, CA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-341103.

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Wilkins, C. G., S. Croft, B. Daniels, and S. Wardle. "Combined HRGS/PNCC Systems for the Assay of Plutonium Contaminated Waste Arising From the Drigg Retrieval Project." In ASME 2003 9th International Conference on Radioactive Waste Management and Environmental Remediation. ASMEDC, 2003. http://dx.doi.org/10.1115/icem2003-4804.

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Between 1959 and 1967, Plutonium Contaminated Material (PCM) was stored in the magazines at the Low Level Waste Facility at Drigg. However, PCM is now classified as Intermediate Level Waste — rather than Low Level Waste — and so a programme to remove the PCM is underway. In support of this programme a suite of safety related non-destructive assay instrumentation has been supplied to the Drigg Site in order to characterise the PCM prior to transportation. Three identical assay systems employing High Resolution Gamma Spectrometry (HRGS) and Passive Neutron Coincidence Counting (PNCC) have been i
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Doucet, M., L. Durand Terrasson, and J. Mouton. "Safety Criticality Standards Using the French CRISTAL Code Package: Application to the AREVA NP UO2 Fuel Fabrication Plant." In 14th International Conference on Nuclear Engineering. ASMEDC, 2006. http://dx.doi.org/10.1115/icone14-89017.

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Criticality safety evaluations implement requirements to proof of sufficient sub critical margins outside of the reactor environment for example in fuel fabrication plants. Basic criticality data (i.e., criticality standards) are used in the determination of sub critical margins for all processes involving plutonium or enriched uranium. There are several criticality international standards, e.g., ARH-600, which is one the US nuclear industry relies on. The French Nuclear Safety Authority (DGSNR and its advising body IRSN) has requested AREVA NP to review the criticality standards used for the
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Informes sobre el tema "Plutonic suite"

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Loveridge, W. D., I. F. Ermanovics, and R. W. Sullivan. U-Pb ages on zircon from the Maggo Gneiss, the Kanairiktok Plutonic Suite and the Island Harbour Plutonic Suite, coast of Labrador, Newfoundland. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1987. http://dx.doi.org/10.4095/122749.

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Emslie, R. F., I. F. Ermanovics, and A. B. Ryan. Geology of the northern Nain Plutonic Suite and its envelope rocks, Labrador. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208648.

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LeCheminant, A. N. Lamprophyre dykes in the Awry plutonic suite, North Arm, Great Slave Lake, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207439.

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Emslie, R. F. Troctolitic rocks of the Reid Brook intrusion, Nain Plutonic Suite, Voisey Bay area, Labrador. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207456.

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Frith, R. A., and O. van Breemen. U-Pb zircon age from the Himag plutonic suite, Thelon Tectonic Zone, Churchill Structural Province, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/129069.

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Corrigan, D., N. Wodicka, I. Lafrance, and D. Bandyayera. Lac Soisson Intrusive Suite: a potential extension of the Nain Plutonic Complex in the western Core Zone, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2019. http://dx.doi.org/10.4095/314596.

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Hamilton, M. A., A. B. Ryan, R. F. Emslie, and I. F. Ermanovics. Identification of Paleoproterozoic anorthositic and monzonitic rocks in the vicinity of the Mesoproterozoic Nain Plutonic Suite, Labrador: U-Pb evidence. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/210053.

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Davidson, A., and O. van Breemen. Age and extent of the Frontenac plutonic suite in the Central metasedimentary belt, Grenville Province, southeastern Ontario; Radiogenic age and isotopic studies: Report 13. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2000. http://dx.doi.org/10.4095/211628.

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Lambert, M. L., and O. Van Breemen. U - Pb Zircon Ages From the Sleepy Dragon Complex and a New Occurrence of Basement Rocks Within the Meander Lake Plutonic Suite, Slave Province, N.w.t. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/131939.

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Woodsworth, G. J., R. G. Anderson, A. Brookfield, and P. Tercier. Distribution of Proterozoic To Miocene Plutonic Suites in the Canadian Cordillera. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1988. http://dx.doi.org/10.4095/130586.

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