Origin of a glacially influenced shallow marine chromite placer, Port au Port Bay, western Newfoundland, Canada
Canadian Journal of Earth Sciences
by Mehmet Duyan, Nick Eyles
1w ago
Canadian Journal of Earth Sciences, Ahead of Print. Detrital chromite is currently accumulating in the wave-influenced gravel-dominated shoreface of eastern Port au Port Bay of western Newfoundland adjacent to the mouth of Fox Island River. Chromium (Cr) concentrations of up to 7485 ppm occur in modern cross-bedded shallow marine gravel and pebbly sand facies sourced from rapidly eroding coastal cliffs cut in a lateglacial and early postglacial fan delta and raised beach facies. These sediments fill a broad coastal embayment and were deposited by a glacially influenced Fox Island River du ..read more
Visit website
Present-day kinematics of the northwest Moroccan Atlantic Margin from GNSS data: west southwest extrusion at the western end of the High Atlas
Canadian Journal of Earth Sciences
by Khalid Lakhouidsi, Abdelali Fadil, Abdelilah Tahayt, Abderrahmane Soulaimani
1w ago
Canadian Journal of Earth Sciences, Ahead of Print. The Global Navigation Satellite System (GNSS) has emerged as a practical and effective technique for studying slow and steady geodynamic movements, enabling continuous monitoring and precise quantification of deformation over different timescales. In Morocco, a network of GNSS stations has been established, offering valuable insights into tectonic processes. This paper focuses on investigating the geodynamic motion of the northwest Moroccan Atlantic Margin. By utilizing GNSS data, subsidence rates and horizontal velocity fields were determine ..read more
Visit website
Sedimentary characteristics, lithofacies, and paleogeography of the Middle–Lower Cambrian in the Tarim Basin, NW China
Canadian Journal of Earth Sciences
by Tianyu Ji, Wei Yang, Xueqiong Wu, Dejiang Li, Mancang Liu, Chengpeng Song, Xi Chen
1w ago
Canadian Journal of Earth Sciences, Ahead of Print. The Cambrian pre-salt dolomite sequence in the Tarim Basin is a target zone of great strategic significance for hydrocarbon exploration in the basin. Using the results of the interpretation of 3D seismic data from Lunnan and 2D seismic data covering the whole basin, and based on a synthesis of outcrop data, drilling data, well logs, core data, and thin-section data, and the findings from previous studies, this paper studies the characteristics of the facies of the Middle–Lower Cambrian in the platform area in the Tarim Basin, the formation an ..read more
Visit website
LA-ICP-MS zircon U–Pb ages, geochemistry, and genesis of Paleozoic granites from Biezhentao Mountain, Western Tianshan, Xinjiang
Canadian Journal of Earth Sciences
by Xiang Li, Fang Xia, Ling-Ling Gao, Chuan Chen, Xiao-Fei Du, Shun-Da Li
1w ago
Canadian Journal of Earth Sciences, Volume 61, Issue 4, Page 505-523, April 2024. The geologic history of the Western Tianshan region is important for understanding the evolution of the Central Asian Orogenic Belt and accretionary orogenesis. Paleozoic and Mesozoic igneous rocks are present along the northern margin of the Yili Block; however, studies of Paleozoic subduction and collisional events have been relatively limited. Published geochronologies of Middle Devonian magmatic rocks in this region are also lacking. Therefore, this study analyzed the zircon U–Pb ages and major and trace elem ..read more
Visit website
Net evolution of subglacial sediment transport in the Quebec–Labrador sector of the Laurentide Ice Sheet
Canadian Journal of Earth Sciences
by Jessey M. Rice, Martin Ross, Heather E. Campbell, Roger C. Paulen, M. Beth McClenaghan
1M ago
Canadian Journal of Earth Sciences, Ahead of Print. The Laurentide Ice Sheet's (LIS) interior had a dynamic polythermal base, but the spatiotemporal variations of subglacial processes related to ice divide migration and other transient changes remain largely unknown, limiting our understanding of regional glacial dynamics. Previous studies focused on the regional glacial landform record, while ice sheet models lacked detailed parameterization within these regions, leading to an overestimation of cold-based subglacial conditions' extent and duration. In this study, glacial sediment dispersal pa ..read more
Visit website
Sulphide petrology and ore genesis of the stratabound Sheep Creek sediment-hosted Zn–Pb–Ag–Sn prospect, and U–Pb zircon constraints on the timing of magmatism in the northern Alaska Range
Canadian Journal of Earth Sciences
by Cynthia Dusel-Bacon, John N. Aleinikoff, Suzanne Paradis, John F. Slack
1M ago
Canadian Journal of Earth Sciences, Ahead of Print. The Sheep Creek prospect is a stratabound Zn–Pb–Ag–Sn massive sulfide occurrence in the Bonnifield mining district, northern Alaska Range. The prospect is within a quartz–sericite–graphite–chlorite schist unit associated with Devonian carbonaceous and siliceous metasedimentary rocks. Volcanogenic massive sulfide (VMS) deposits in the district are hosted in felsic metavolcanic rocks (362 ± 2 Ma) associated with siliciclastic and carbonaceous sedimentary rocks that overlie the stratigraphic sequence hosting the Sheep Creek prospect. F ..read more
Visit website
Assessing the relative threats from Canadian volcanoes
Canadian Journal of Earth Sciences
by Melanie C. Kelman, Alexander M. Wilson
2M ago
Canadian Journal of Earth Sciences, Ahead of Print. We assessed 28 Canadian volcanoes in terms of their relative threats to people, aviation, and infrastructure. The methodology we used was developed by the United States Geological Survey for the 2005 National Volcano Early Warning System. Each volcano is scored on multiple hazard and exposure factors, producing an overall threat score. The scored volcanoes are assigned to five threat categories, ranging from Very Low to Very High. We developed a knowledge uncertainty score to provide additional information about assessed threat levels; this d ..read more
Visit website
The influence of fluvial and glacial watershed dynamics on Holocene sediment accumulation in Cariboo Lake, Columbia Mountains, British Columbia, Canada
Canadian Journal of Earth Sciences
by A. Cebulski, J. Desloges
2M ago
Canadian Journal of Earth Sciences, Ahead of Print. Records of sedimentation collected from Cariboo Lake, situated in the northern Columbia Mountains, British Columbia, Canada, are analyzed to assess Holocene fluvial and glacial watershed dynamics. The aim of this study is to provide a proxy record of Holocene hydroclimate and glacier change from sediment archives at a higher temporal resolution compared to available records for the Interior Ranges of British Columbia. Deglacial and Holocene sediment accumulation is observed to reach a maximum thickness of 35 m in deep parts of the lake, using ..read more
Visit website
Analysis of the late Hirnantian and early Rhuddanian unconformities of southern Ontario: evidence for far-field glacioeustatic effects
Canadian Journal of Earth Sciences
by C.A. Farnam, C.E. Brett
2M ago
Canadian Journal of Earth Sciences, Ahead of Print. Several unconformities have been previously recognized in the Late Ordovician and early Silurian strata of southern Ontario. We examined the Georgian Bay, Queenston, Whirlpool, Manitoulin, Power Glen, and Cabot Head formations and associated unconformities. Detailed sequence stratigraphic and chemostratigraphic analysis of Late Ordovician and early Silurian outcrops between Niagara, New York, and Manitoulin Island, Ontario, reveals new insights on the timing of the erosional unconformities and the Ordovician–Silurian boundary. We recognize th ..read more
Visit website
Exploring the Moho beneath the Northern Canadian Cordillera, with seismically constrained gravity inversion
Canadian Journal of Earth Sciences
by Nathan Hayward, Ernst Schetselaar
2M ago
Canadian Journal of Earth Sciences, Ahead of Print. The geometry and depth of the Moho beneath the Northern Canadian Cordillera and adjacent North American craton are modeled through the application of both cokriging and 3-D inversion of gravity data, integrated with sparse seismic depth estimates. Models require a regional density correction, with lower densities beneath the Cordillera than the craton. The lower densities are primarily attributed to a reduction in upper mantle density, ascribed to thermal expansion under regionally higher temperatures. The eastern margin of this low-density z ..read more
Visit website

Follow Canadian Journal of Earth Sciences on FeedSpot

Continue with Google
Continue with Apple
OR