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Recent Articles in Sedimentology
Suspended Sediment Concentrations In Three Tributaries Of The Little River, Chaney Swiney
University of Tennessee, Knoxville
Suspended Sediment Concentrations In Three Tributaries Of The Little River, Chaney Swiney
University of Tennessee Honors Thesis Projects
No abstract provided.
Tectonic Shifts: Haiti Since The Earthquake, Toni Pressley-Sanon
University of Massachusetts - Amherst
Tectonic Shifts: Haiti Since The Earthquake, Toni Pressley-Sanon
African Diaspora Archaeology Newsletter
There have been several publications about Haiti since the earthquake devastated the tiny island nation in January 2010. Many of them, especially those that have come from people who have a long history with Haiti, have been collaborations as the authors/editors have culled from the Haitian cultural tradition of the kombit as a way of conceptualizing and framing their projects. Mark Schuller and Pablo Morales’ co-edited volume, Tectonic Shifts: Haiti Since the Earthquake (2012), is one of the latest incarnations of this trend. The text gathers together a diverse group of scholars and grassroots activists to create a comprehensive ...
Chemostratigraphy Of The Early Pliocene Diatomite Interval From Mis And-1b Core (Antarctica): Paleoenvironment Implications, Giovanna Scopelliti, Adriana Bellanca, Donata Monien, Gerhard Kuhn
University of Nebraska - Lincoln
Chemostratigraphy Of The Early Pliocene Diatomite Interval From Mis And-1b Core (Antarctica): Paleoenvironment Implications, Giovanna Scopelliti, Adriana Bellanca, Donata Monien, Gerhard Kuhn
ANDRILL Research and Publications
The AND-1B drill core (1285 m-long) was recovered, inside the ANDRILL (ANtarctic geological DRILLing) Program, during the austral summer of 2006/07 from beneath the floating McMurdo Ice Shelf. Drilling recovered a stratigraphic succession of alternating diamictites, diatomites and volcaniclastic sediments spanning about the last 14 Ma. A core portion between 350 and 480 mbsf, including a 80 m-thick diatomite interval recording the early Pliocene warming event, was investigated in term of opal biogenic content and element geochemistry. Across the diatomite interval, in spite of the lithological uniformity, a fluctuating biogenic opal profile mirrors the δ18O record, testifying a decrease ...
Clay Synthesis: Modeling The Uptake Of Potassium During Low Temperature Illitization Of Smectite, Peter M. Razumov, Lucy C. Taylor, Rebecca A. Pickering
Georgia State University
Clay Synthesis: Modeling The Uptake Of Potassium During Low Temperature Illitization Of Smectite, Peter M. Razumov, Lucy C. Taylor, Rebecca A. Pickering
Georgia State Undergraduate Research Conference
No abstract provided.
Formation And Alteration Of Basaltic Soils On Mars, Ian Oliver McGlynn
University of Tennessee, Knoxville
Formation And Alteration Of Basaltic Soils On Mars, Ian Oliver Mcglynn
Doctoral Dissertations
The current surface of Mars is an arid inhospitable environment, dominated by aeolian processes, composed of largely volcanic rocks that have little apparent indication of pervasive aqueous chemical weathering, and blanketed by dust. Rocks are composed of basalts and the “soil” sediments appear to be largely basaltic-derived, and are chemically similar on a global scale. If the climate was once warmer and wetter during the Noachian period, with environmental conditions favorable to the development of life, physically weathered remnants, such as large quantities of phyllosilicate minerals, should remain. Basaltic soils provide a crucial constraint on chemical and physical weathering processes ...
Provenance And Geological Significance Of Red Mud And Other Clastic Sediments Of The Mugnano Cave (Montagnola Senese, Italy), Francesco Iacoviello, Ivan Martini
University of South Florida
Provenance And Geological Significance Of Red Mud And Other Clastic Sediments Of The Mugnano Cave (Montagnola Senese, Italy), Francesco Iacoviello, Ivan Martini
International Journal of Speleology
The Mugnano cave is characterized by a thick clastic sedimentary fill showing a great variability of sedimentary facies, ranging from clay to coarse-grained sand deposits. This paper deals with combined sedimentological and mineralogical (XRD and SEM) studies of these sediments and bedrock insoluble residues in order to understand the origin and geological significance of cave deposits, with particular attention to red mud sediments, often considered as the residue of host rock dissolution. Three different sedimentary facies were recognized: i) YS, yellow sand with occasionally shell fragments, testifying the arrival of sediments from the surrounding landscape; ii) RS, red laminated mud ...
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A Sedimentological Study Of Modern And Ancient Lacustrine Environments At Michael Bay, Lake Huron
Provenance And Geological Significance Of Red Mud And Other Clastic Sediments Of The Mugnano Cave (Montagnola Senese, Italy), Francesco Iacoviello, Ivan Martini
Responses Of Palau's Coral Reefs To Disturbances At Multiple Scales, Yimnang Golbuu
Reservoir Characterization And Enhanced Oil Recovery Potential In Middle Devonian Dundee Limestone Reservoirs, Michigan Basin, Usa, Abrahim Abduslam
Chemostratigraphy Of The Early Pliocene Diatomite Interval From Mis And-1b Core (Antarctica): Paleoenvironment Implications, Adriana Bellanca, Donata Monien, G. Kuhn, Giovanna Scopelliti
Sedimentary Petrology And Provenance Of The Teddy Creek Group Sw Montana
Ice-Core Dating And Chemistry By Direct-Current Electrical Conductivity, Paul Mayewski
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