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Статті в журналах з теми "Bulk rock Sm-Nd"
ALI, K., A. ANDRESEN, W. I. MANTON, R. J. STERN, S. A. OMAR, and A. E. MAURICE. "U–Pb zircon dating and Sr–Nd–Hf isotopic evidence to support a juvenile origin of the ~ 634 Ma El Shalul granitic gneiss dome, Arabian–Nubian Shield." Geological Magazine 149, no. 5 (December 16, 2011): 783–97. http://dx.doi.org/10.1017/s0016756811000975.
Повний текст джерелаStevenson, Ross K., P. J. Patchett, and R. F. Martin. "Sm–Nd isochron from a granodiorite–granite complex in the Portman Lake region, Northwest Territories." Canadian Journal of Earth Sciences 26, no. 12 (December 1, 1989): 2724–29. http://dx.doi.org/10.1139/e89-232.
Повний текст джерелаDemonterova, Elena I., Alexei V. Ivanov, Ekaterina M. Mikheeva, Anastasia V. Arzhannikova, Andrei O. Frolov, Sergei G. Arzannikov, Nikolai V. Bryanskiy, and Lyudmila A. Pavlova. "Early to Middle Jurassic history of the southern Siberian continent (Transbaikalia) recorded in sediments of the Siberian Craton: Sm-Nd and U-Pb provenance study." Bulletin de la Société géologique de France 188, no. 1-2 (2017): 8. http://dx.doi.org/10.1051/bsgf/2017009.
Повний текст джерелаManeiro, Kathryn A., Ethan F. Baxter, Scott D. Samson, Horst R. Marschall, and Jack Hietpas. "Detrital garnet geochronology: Application in tributaries of the French Broad River, Southern Appalachian Mountains, USA." Geology 47, no. 12 (October 15, 2019): 1189–92. http://dx.doi.org/10.1130/g46840.1.
Повний текст джерелаMikhalsky, E. V., A. A. Laiba, B. V. Beliatsky, and K. Stüwe. "Geology, age and origin of the Mount Willing area (Prince Charles Mountains, East Antarctica)." Antarctic Science 11, no. 3 (September 1999): 338–52. http://dx.doi.org/10.1017/s0954102099000437.
Повний текст джерелаWindom, Kenneth E., W. Randall Van Schmus, Karl E. Seifert, E. Timothy Wallin, and Raymond R. Anderson. "Archean and Proterozoic tectono-magmatic activity along the southern margin of the Superior Province in northwestern Iowa, United States." Canadian Journal of Earth Sciences 30, no. 6 (June 1, 1993): 1275–85. http://dx.doi.org/10.1139/e93-109.
Повний текст джерелаMitchell, Roger H. "Igneous Rock Associations 26. Lamproites, Exotic Potassic Alkaline Rocks: A Review of their Nomenclature, Characterization and Origins." Geoscience Canada 47, no. 3 (September 28, 2020): 119–42. http://dx.doi.org/10.12789/geocanj.2020.47.162.
Повний текст джерелаSushchevskaya, N. M., T. A. Shishkina, M. V. Portnyagin, V. G. Batanova, and B. V. Belyatsky. "Long-lasting influence of the Discovery plume on tholeiitic magmatism in the South Atlantic: data on basalts recovered by hole 513a, dsdp leg 71." Геохимия 64, no. 2 (March 15, 2019): 107–27. http://dx.doi.org/10.31857/s0016-7525642107-127.
Повний текст джерелаSaleeby, Jason B. "Age and tectonic setting of the Duke Island ultramafic intrusion, southeast Alaska." Canadian Journal of Earth Sciences 29, no. 3 (March 1, 1992): 506–22. http://dx.doi.org/10.1139/e92-044.
Повний текст джерелаShaw, D. M., A. P. Dickin, H. Li, R. H. McNutt, H. P. Schwarcz, and M. G. Truscott. "Crustal geochemistry in the Wawa–Foleyet region, Ontario." Canadian Journal of Earth Sciences 31, no. 7 (July 1, 1994): 1104–21. http://dx.doi.org/10.1139/e94-099.
Повний текст джерелаДисертації з теми "Bulk rock Sm-Nd"
Chaumba, Jefferson B. "The Russell Lake Allochthon, southern Appalachians structure, petrography, bulk-rock and mineral chemistry, O, H, and Sm-Nd isotope geochemistry /." 2009. http://purl.galileo.usg.edu/uga%5Fetd/chaumba%5Fjefferson%5Fb%5F200908%5Fphd.
Повний текст джерелаDirected by Michael Roden. For abstract see https://getd.libs.uga.edu/pdfs/chaumba%5Fjefferson%5Fb%5F200908%5Fphd.pdf. Includes bibliographical references (leaves 246-279).
Job, A. L. "Evolution of the basal Adelaidean in the northern Flinders Ranges: deposition, provenance and deformation of the Callanna and lower Burra Groups." Thesis, 2011. http://hdl.handle.net/2440/96175.
Повний текст джерелаThe rift and deformational evolution of the Adelaide Fold Belt’s northern-most extent, the northern Flinders Ranges, has received comparatively little attention than that of the southern Adelaide Fold Belt. The Arkaroola area, located in the mid-north northern Flinders Ranges, exposes the lowermost Adelaidean stratigraphy of this rift complex, the Callanna and lower Burra Groups, in a near complete sedimentary sequence. The rift history of this stratigraphy is complex, with deposition being largely controlled by the northeast-southwest orientated Paralana Fault and similarly orientated local growth faults. Locally, the Paralana Fault deviates from its regional orientation and forms a north-south striking segment, which under a considered sinistral strike-slip regime during extension would potentially create localised transtension in a ‘releasing bend’ environment. Rifting in the Arkaroola area is therefore considered to be analogous to the formation of a pull-apart basin. U-Pb dating of detrital zircons from the Paralana Quartzite, Humanity Seat Formation and Blue Mine Conglomerate from the Callanna and lower Burra groups yields ages that are comparable to local source regions the Gawler Craton, Mount Painter Basement Complex and the Curnamona Province, and suggest proximal derivation during early rift phases. Sm-Nd bulk rock analysis on the finer grained Woodnamoka Formation implies derivation from the Mount Painter Basement Complex or the upper Willyama Supergroup of the Curnamona Province, the latter of which potentially suggests a more distal provenance region outside of the Australian continent. Deformation in the northern Flinders Ranges has previously been largely ascribed to the ca. 500 Ma Delamerian Orogeny. However, the Arkaroola area exhibits complex deformation not observed in the directly overlying gently folded stratigraphy. Reactivation of pull-apart rift structures during transpression is considered a possible mechanism for producing and localising such deformation. The possibility of an early Neoproterozoic deformational event occurring prior to deposition of the lesser-deformed overlying stratigraphy is also considered, but in lieu of an unequivocal orogenic unconformity, cannot be confidently ascribed. Temporal constraints defined by this study are too broad to accurately define the timing of deformation, and therefore its timing and potential relationship to the Delamerian Orogeny remains largely enigmatic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011