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Browsing by Author "Pe-Piper, Georgia"
Now showing items 1-20 of 27
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(Halifax, N.S. : Saint Mary's University, 2019)Forward stratigraphic modelling of the central Scotian Basin is used to evaluate proposed provenance pathways in the Early Cretaceous and exploration risk. Modelling results confirm proposed pathways, supporting the diversion ...
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Chlorite diagenesis in reservoir sandstones of the Lower Missisauga formation, offshore Nova Scotia (Halifax, N.S. : Saint Mary's University, 2007)Diagenetic chlorite rims on quartz grains preserve porosity by preventing the formation of secondary, pore-filling quartz overgrowths in wells from the Venture and Thebaud fields. Elsewhere, in the Norwegian Sea and the ...
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(Halifax, N.S. : Saint Mary's University, 2010)Early Cretaceous tectonism and volcanism is widespread in the eastern Mesozoic-Cenozoic Scotian Basin. The precise stratigraphic position of volcanic rocks within wells has been re-evaluated and the volcanological character ...
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(Halifax, N.S. : Saint Mary's University, 2019)There were two main objectives for this study. The first, to understand the detrital mineral assemblages at different depths in a group of wells in the Central Scotian Basin, eastern Canada. The second, to determine the ...
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(Halifax, N.S. : Saint Mary's University, 2018)Provenance and diagenesis are important processes to study in order to determine reservoir potential of sandstones within a sedimentary basin. The Scotian Basin is a large sedimentary basin located off the eastern part ...
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(Halifax, N.S. : Saint Mary's University, 2015)Diagenetic processes can be studied to determine the oil and gas reservoir potential within a sedimentary basin. The majority of focus within the Scotian Basin has been on Lower Cretaceous sandstones, with minimal studies ...
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(Halifax, N.S. : Saint Mary's University, 2017)The hypothesis of sediment supply to the SW Scotian Basin from the diversion of the Sable River through the Fundy Basin was tested based on sand provenance of the COST G-2 well and regional correlation of the Naskapi Member. ...
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(Slovak Academy of Sciences Geological Institute, 2014-06)Paleocene to Oligocene tectonic processes in northwest Iran resulted in extensive I-type calc-alkaline and alkaline magmatic activity in the Ahar region. Numerous skarn deposits formed in the contact between Upper ...
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(Halifax, N.S. : Saint Mary's University, 2018)This study was conducted on the Notre Dame Trough (NDT) on the Northeast Newfoundland Shelf. The purpose of this project was to help unravel the glacial history, including the timing of a large slide block in the NDT, and ...
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(Halifax, N.S. : Saint Mary's University, 2017)The Sigri Pyroclastic Formation in the western side of the island of Lesbos consists primarily of pumice flows, mud flows and stream conglomerate. Most of the pyroclastic rocks appear to be derived from a caldera near ...
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(Halifax, N.S. : Saint Mary's University, 2022-12-20)Kaolin is found along the south-eastern contact of the South Mountain Batholith and the Meguma metasediments, 21 km along length on strike of the Tobeatic shear zone and on trend with regional folds and faults. The Meguma ...
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(Elsevier, 2019-05-17)Data available from a detailed mineralogical investigation of the Petrified Forest of Lesbos and its host pyroclastic rocks [1] are summarized and a link is provided to the full data at https://data.mendeley.com/datasets ...
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(Halifax, N.S. : Saint Mary's University, 2015)The Cretaceous was a time when global temperatures and rainfall patterns were controlled by plate tectonic changes and intense volcanic activity. High temperatures, high weathering rates and unusual ocean circulation ...
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(American Geophysical Union, 2014-12)The Baijiantan and Darbut ophiolites in West Junggar are exposed in steep fault zones (>70°) containing serpentinite mélange, in contact on either side with regionally distributed Upper Devonian-Lower ...
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(Halifax, N.S. : Saint Mary's University, 2012)Upper Jurassic–Lower Cretaceous shales of the Scotian Basin, offshore Nova Scotia, are a primary source of hydrocarbons and of the basinal fluids that affected diagenesis of sandstone reservoirs. This study documents and ...
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(Halifax, N.S. : Saint Mary's University, 2011)The Wentworth Pluton is a bimodal intrusion which consists principally of a 362 Ma, A-type granite, part of which was remelted by a major gabbro intrusion, resulting in the formation of late granites. REE- rare metal ...
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(Halifax, N.S. : Saint Mary's University, 2013)The Porter Puddle Complex (PPC) of the Ordovician–Silurian Marmot Formation volcanics (MFV) is located in the northeastern Canadian Cordillera (NTS map sheet 106B/SE). The PPC has previously been interpreted as a rift-related ...
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(Halifax, N.S. : Saint Mary's University, 2020)Forward stratigraphic modeling has been performed on the SW Scotian Basin in order to understand the geological evolution, sediment distribution, and deep-water clastic reservoir quality in the area. The SW Scotian Basin ...
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(Halifax, N.S. : Saint Mary's University, 2015)Mid Jurassic to Lower Cretaceous clastic deposits in the SW Scotian Basin are poorly known and understood. Detrital mineral chemistry was used to determine their provenance, whereas chemical composition of diagenetic ...
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(Halifax, N.S. : Saint Mary's University, 2016)Newburn H-23 is one of seven deep wells drilled on the Scotian Slope. These wells are new and thus in the early stages of research. As such it is important to determine the history of the detrital and diagenetic minerals ...
Now showing items 1-20 of 27