Geological Controls On Reservoir Quality And Geologic Carbon Sequestration Potential In The Upper Cambrian Mount Simon Sandstone,
2011
Western Michigan University
Geological Controls On Reservoir Quality And Geologic Carbon Sequestration Potential In The Upper Cambrian Mount Simon Sandstone, Kyle Patterson
Masters Theses
The Upper (?) Cambrian Mount Simon Sandstone is an important deep saline geological carbon sequestration (GCS) target throughout the Midwest, USA. The distribution of sedimentary facies, primary mineralogy, and diagenetic alterations and the relationship to wireline log response and reservoir quality throughout the Michigan basin are not well known. This study uses rock core, thin section point counts, x-ray diffraction, inferred spectroscopy, conventional core plug porosity and permeability and pressure fall-off test data to constrain wireline log interpretations of regional geology and reservoir quality.
Prior to the permitting of a CO2 sequestration project, documentation of a robust transient injection …
Relation Of Recent Seismicity (1988-Present) To The 1958 Huslia, Alaska Earthquake Sequence,
2011
Department of Geological Sciences, University of Texas at ElPaso
Relation Of Recent Seismicity (1988-Present) To The 1958 Huslia, Alaska Earthquake Sequence, Abigail Monreal^, Diane I. Doser*
COURI Symposium Abstracts, Spring 2011
We have examined how recent seismicity in the Huslia region of central Alaska is related to active faults and the 1958 earthquake sequence (with at least 3 events of magnitude >6). Most of this region is swampy lowland dominated by alluvial material deposited by the Koyukuk River, making surficial identification of active faults difficult. This portion of Alaska is also of interest because it appears to be a region in transition between the strike-slip faulting of the Salcha-Fairbanks-Minto Flats seismic zone and normal faulting of western Alaska (Norton Sound/Seward Peninsula). Researchers have suggested this change in the nature of faulting …
Middle To Late Miocene Extremely Rapid Exhumation And Thermal Reequilibration In The Kung Co Rift, Southern Tibet,
2011
Central Washington University
Middle To Late Miocene Extremely Rapid Exhumation And Thermal Reequilibration In The Kung Co Rift, Southern Tibet, Jeffrey Lee, Christian Hager, Simon R. Wallis, Daniel F. Stockli, Martin J. Whitehouse, Mutsuki Aoya, Yu Wang
All Faculty Scholarship for the College of the Sciences
The Kung Co rift is an approximately NNW striking, WSW dipping normal fault exposed in southern Tibet and is part of an extensive network of active approximately NS striking normal faults exposed across the Tibetan Plateau. Detailed new and published (U-Th)/He zircon and apatite thermochronometric data from the footwall of the early Miocene Kung Co granite provide constraints on the middle Miocene to present-day exhumation history of the footwall to the Kung Co fault. Inverse modeling of thermochronometric data yield age patterns that are interpreted as indicating (1) initiation of normal fault slip at ∼12–13 Ma and rapid exhumation of …
Mapping Unmarked Graves In The Mescalero Apache Indian Reservation,
2011
Department of Geological Sciences, University of Texas at El Paso
Mapping Unmarked Graves In The Mescalero Apache Indian Reservation, Ashley Galusina Nauer^, Stephanie Chavez^, Laura Serpa*
COURI Symposium Abstracts, Spring 2011
Citizens living on the Apache Indian Reservation in Mescalero, New Mexico have experienced difficulty in burying their dead because when they dig a new grave, they often find a body from an earlier burial. The reservation does not have rigorous rules on locating and marking graves and, thus, there are numerous unmarked burial sites within and outside of the existing cemeteries. Officials from the reservation approached the Geological Sciences Department for assistance to map grave locations in the area’s three graveyards. In this project, we will use shallow ground-penetrating radar (GPR) to find the graves and digital global positioning system …
Studies Of Seismicity Near The Active Volcano Mt. Spurr,
2011
Department of Geological Sciences, University of Texas at El Paso
Studies Of Seismicity Near The Active Volcano Mt. Spurr, Sarah J. Olivas^, Diane I. Doser*
COURI Symposium Abstracts, Spring 2011
Seismicity patterns and fault orientations can indicate local stress fields related to volcanic eruptions. There have been many moderate magnitude, shallow earthquakes occurring in the Strandline Lake region about 100km from Anchorage, Alaska near the active volcano, Mt. Spurr. Previous researchers have found that the local stress under Mt. Spurr, before and after its 1992 eruption (1992-1997), differed from the regional stresses, which are related to subduction of the Pacific Plate and Yakutat micro plate. We are analyzing location and patterns of earthquakes occurring since 1998 to determine if more recent seismicity is similar to that occurring before or after …
Seismic Study Of Carlsbad, Nm,
2011
University of Texas at El Paso
Seismic Study Of Carlsbad, Nm, Steven M. Espinosa^, Aaron A. Velasco*
COURI Symposium Abstracts, Spring 2011
Since January 1, 2000, there have been numerous earthquakes recorded in the vicinity of Carlsbad, NM. Importantly, these shallow (10km) earthquakes with magnitudes < 4.3, do not have a fault or system of faults directly mapped to explain these events. We will be relocating the largest and most recent earthquake, which occurred 25km west of Carlsbad, NM of magnitude 4.1 on March 28, 2010. Data recorded by seismic stations from the USArray, a large National Science Foundation project, and our local Kidd Observatory will be used for this analysis. The use of Standing Order of Data (SOD) allows us access seismograms, and the Seismic Analysis Code (SAC) helps in the analysis of the seismic data. We will correlate the hypocenters of aftershocks to the main event hypocenter, allowing us to identify the fault plane. Once a fault plane has been identified, we will begin work on relocating a second event, thereby identifying the responsible faults. We believe that faulting in this area is related to the Rio Grande Rift extension and can be used as evidence for an active rift.
Detecting Unmarked Graves Using Gpr At The Mescalero Apache Reservation,
2011
Department of Geological Sciences, University of Texas at El Paso
Detecting Unmarked Graves Using Gpr At The Mescalero Apache Reservation, Stephanie Y. Chavez^, Ashley G. Nauer, Laura Serpa*
COURI Symposium Abstracts, Spring 2011
In Mescalero, New Mexico, on an Apache Indian Reservation, we were asked to survey the Mescalero Cemetery in order to locate unmarked graves. Back in the late 1800’s, proper documentation of graves was never made. As a result, what is thought to be a new potential burial site is discovered to be an old undocumented grave. Reservation officials have asked us to survey the cemetery and document exact locations of unmarked graves. To achieve this goal, we will use ground penetrating radar (GPR) and a differential global positioning system (DGPS). The collected data will be processed by using EKKO-Mapper and …
Evolution And Emergence Of The Hinterland In The Active Banda Arc-Continent Collision: Insights From The Metamorphic Rocks And Coral Terraces Of Kisar, Indonesia,
2011
Brigham Young University - Provo
Evolution And Emergence Of The Hinterland In The Active Banda Arc-Continent Collision: Insights From The Metamorphic Rocks And Coral Terraces Of Kisar, Indonesia, Jonathan R. Major
Theses and Dissertations
Coral terrace surveys and U-series ages of coral and mollusk shells yield a surface uplift rate of ~0.6 m/ka for Kisar Island. The small island is located NE of Timor in the active Banda Arc of Indonesia. Based on this rate, Kisar first emerged from the ocean as recently as ~450 ka. Terrace surveys show warping that follows a pattern of east-west striking folds, which are along strike of thrust-related folds of similar wavelength imaged by a seismic reflection profile just offshore. This deformation shows that the emergence of Kisar can be attributed to forearc closure along the south-dipping Kisar …
Identifying Complex Fluvial Sandstone Reservoirs Using Core, Well Log, And 3d Seismic Data: Cretaceous Cedar Mountain And Dakota Formations, Southern Uinta Basin, Utah.,
2011
Brigham Young University - Provo
Identifying Complex Fluvial Sandstone Reservoirs Using Core, Well Log, And 3d Seismic Data: Cretaceous Cedar Mountain And Dakota Formations, Southern Uinta Basin, Utah., William H. Hokanson
Theses and Dissertations
The Cedar Mountain and Dakota Formations are significant gas producers in the southern Uinta Basin of Utah. To date, however, predicting the stratigraphic distribution and lateral extent of potential gas-bearing channel sandstone reservoirs in these fluvial units has proven difficult due to their complex architecture, and the limited spacing of wells in the region. A new strategy to correlate the Cedar Mountain and Dakota Formations has been developed using core, well-log, and 3D seismic data. The detailed stratigraphy and sedimentology of the interval were interpreted using descriptions of a near continuous core of the Dakota Formation from the study area. …
Facies Analysis And Reservoir Characterization Of Subtidal, Intertidal, And Supratidal Zones Of The Mudstone-Rich Entrada Sandstone, South-Central Utah,
2011
Brigham Young University - Provo
Facies Analysis And Reservoir Characterization Of Subtidal, Intertidal, And Supratidal Zones Of The Mudstone-Rich Entrada Sandstone, South-Central Utah, Tanner Charles Hicks
Theses and Dissertations
Understanding thickness variation and facies transitions in the mudstone-rich part of the Upper Middle Jurassic (Callovian) Entrada Sandstone depositional system is critical for constraining the paleogeography and evaluating the economic potential of Utah's Entrada Sandstone. Facies of the Entrada Sandstone in south-central Utah are dominated by mudstone-rich intertidal facies that were widespread within the Jurassic seaway. Intertidal deposits interfinger basinward with subtidal ooid-bearing shoals and bars, and landward supratidal sabkha, and erg-margin eolian deposits. Three sections were measured to improve understanding of the lateral and vertical facies transitions. Variations in thickness indicate the rate of developing accommodation space was high …
Evidence Of Tectonic Uplift Along The Oceanic Fault Near San Simeon, San Luis Obispo County, California,
2011
California Polytechnic State University, San Luis Obispo
Evidence Of Tectonic Uplift Along The Oceanic Fault Near San Simeon, San Luis Obispo County, California, George Gecy
Earth and Soil Sciences
Post-Seismic satellite imagery after the 2003 earthquake near San Simeon confirmed 10s of millimeters of north-east side uplift along the Oceanic Fault. In order to determine whether or not there has been a history of tectonic uplift northeast of the Oceanic Fault zone, longitudinal profiles of Morro Creek and San Simeon were made using a digital planimeter and 1:24,000 scale maps. Utilizing the stream profiles, convexities could be observed in the streams coinciding where the streams crossed the Oceanic Fault; of the stream profiles, the convexity along San Simeon Creek could be confirmed to be caused by north-east side uplift …
Sphenothallus-Like Fossils From The Martinsburg Formation (Upper Ordovician), Tennessee, Usa,
2011
Smith College
Sphenothallus-Like Fossils From The Martinsburg Formation (Upper Ordovician), Tennessee, Usa, Maya Li Wei-Haas, Bosiljka Glumac, H. Allen Curran
Geosciences: Faculty Publications
Tubular fossils, up to 2 mm in diameter and 60 mm in length, occur rarely in the upper Martinsburg Formation (Upper Ordovician), northeastern Tennessee Appalachians, U.S.A. The fossils are unbranched, straight or slightly bent, occasionally twisted and wrinkled, and not significantly tapered. Orientation of the fossils within shallow-marine tempestites suggests that they represent remains of organisms that were broken, transported, and deposited by storm waves and currents. The fossils are morphologically similar to many of the previously identified species belonging to the genus Sphenothallus, a relatively rare tube-dwelling Paleozoic marine invertebrate. Owing to the limited evidence for distal widening of …
Recent Increase In Black Carbon Concentrations From A Mt. Everest Ice Core Spanning 1860-2000 Ad,
2011
Central Washington University
Recent Increase In Black Carbon Concentrations From A Mt. Everest Ice Core Spanning 1860-2000 Ad, Susan D. Kaspari, M. Schwikowski, M. Gysel, M. G. Flanner, S. Kang, S. Hou, P. A. Mayewski
All Faculty Scholarship for the College of the Sciences
A Mt. Everest ice core spanning 1860–2000 AD and analyzed at high resolution for black carbon (BC) using a Single Particle Soot Photometer (SP2) demonstrates strong seasonality, with peak concentrations during the winter‐spring, and low concentrations during the summer monsoon season. BC concentrations from 1975–2000 relative to 1860–1975 have increased approximately threefold, indicating that BC from anthropogenic sources is being transported to high elevation regions of the Himalaya. The timing of the increase in BC is consistent with BC emission inventory data from South Asia and the Middle East, however since 1990 the ice core BC record does not indicate …
Partitioning Of Localized And Diffuse Deformation In The Tibetan Plateau From Joint Inversions Of Geologic And Geodetic Observations,
2011
Smith College
Partitioning Of Localized And Diffuse Deformation In The Tibetan Plateau From Joint Inversions Of Geologic And Geodetic Observations, John P. Loveless, Brendan J. Meade
Geosciences: Faculty Publications
The spatial complexity of continental deformation in the greater Tibetan Plateau region can be defined as the extent to which relative motion of the Indian and Asian plates is partitioned between localized slip on major faults and distributed deformation. Potency rates provide a quantitative metric for determining the magnitudes of diffuse and on-fault crustal deformation, which are proportional to strain rates within crustal micro-plates and fault slip rates, respectively. We simultaneously estimate micro-plate rotation rates, interseismic elastic strain accumulation, fault slip rates on major structures, and strain rates within 24 tectonic micro-plates inferred from active fault maps in the greater …
Petrographic Comparison And Contrast Of Fluvial And Deltaic Sandstones, Upper Pennsylvanian Oread Cyclothem, Ne Oklahoma,
2011
Missouri University of Science and Technology
Petrographic Comparison And Contrast Of Fluvial And Deltaic Sandstones, Upper Pennsylvanian Oread Cyclothem, Ne Oklahoma, Jonathan Obrist-Farner, Wan Yang
Geosciences and Geological and Petroleum Engineering Faculty Research & Creative Works
Upper Pennsylvanian sandstones have been the target in petroleum exploration and production in Kansas and Oklahoma. However, the petrographic characteristics of these sandstones have been rarely reported. A good understanding of the characteristics and depositional environments of those sandstones will help explore the correlative subsurface petroleum reservoirs efficiently.
Secondary Minerals From Extrapedogenic Per Latus Acidic Weathering Environments At Geomorphic Edges, Eastern Nebraska, Usa,
2011
University of Nebraska - Lincoln
Secondary Minerals From Extrapedogenic Per Latus Acidic Weathering Environments At Geomorphic Edges, Eastern Nebraska, Usa, Robert Matthew Joeckel, K.D. Wally, B.J. Ang Clement, P.R. Hanson, J.S. Dillon, S.K. Wilson
Conservation and Survey Division: Faculty and Staff Publications
Acidic weathering of the sulfidic Upper Cretaceous Carlile and Pierre Shales in Nebraska has led to the precipitation of the Al sulfate–hydroxide minerals aluminite, alunite, “basaluminite”/felsöbányaite (e.g.,), the aluminum hydroxides gibbsite and bayerite, and the rare Al phosphate hydroxide vashegyite. Kaolinite has also been produced as a result of this acidic weathering. These minerals do not appear as neoformed constituents in any extant soils in the region, and their existence underscores the ability of pyrite oxidation to produce major changes in mineralogy on a Holocene to Recent time scale. Jarosite, hydronium jarosite, gypsum, halotrichite, and melanterite also appear as secondary …
Reproduction And Genetic Detection Of Veligers In Changing Dreissena Populations In The Great Lakes,
2011
Department of Physiology, Wayne State University, Detroit, MI
Reproduction And Genetic Detection Of Veligers In Changing Dreissena Populations In The Great Lakes, Jeffrey L. Ram, Aos S. Karim, Payel Acharya, Pranav Jagtap, Sonal Purohit, Donna R. Kashian
Environmental Science and Geology Faculty Research Publications
Dreissenid bivalves, Dreissena polymorpha (zebra mussel) and Dreissena bugensis (quagga mussel) are biofouling species that invaded the Great Lakes region of North America from source populations in Europe in the 1980s. Initially, D. polymorpha spread faster and farther; however, D. bugensis have recently displaced D. polymorpha in many areas of the Great Lakes and was the first to be found west of the Continental Divide. Early detection of dreissenids is important in anticipating and preventing potentially high economic impacts. To study population dynamics and to enhance detection methods, we assessed “spawnability” using a serotonin bioassay and developed a new, sensitive, …
Lineament Mapping For Groundwater Exploration Using Remotely Sensed Imagery In A Karst Terrain : Rio Tanama And Rio De Arecibo Basins In The Northern Karst Of Puerto Rico,
2011
Michigan Technological University
Lineament Mapping For Groundwater Exploration Using Remotely Sensed Imagery In A Karst Terrain : Rio Tanama And Rio De Arecibo Basins In The Northern Karst Of Puerto Rico, Carla A. Alonso-Contes
Dissertations, Master's Theses and Master's Reports - Open
Remote sensing and advanced digital image processing techniques were developed and tested for delineating karst features important for the subterranean hydrology in the Tanamá River and Rio Grande de Arecibo catchments located in the North Coast Tertiary Basin of Puerto Rico, where groundwater contributes to base flow for surface water bodies which in itself is the main supply of drinking water. This aquifer region is a karst platform of carbonate rocks and clastic beds, thought to comprise a confined aquifer beneath and an unconfined aquifer. Products derived from ASTER, Landsat (ETM+ and TM), a NED DEM (30 m), and a …
Characterization Of Harmonic Tremor At Santiaguito Volcano And Its Implications For Eruption Mechanisms ,
2011
Michigan Technological University
Characterization Of Harmonic Tremor At Santiaguito Volcano And Its Implications For Eruption Mechanisms , Kyle Arthur Brill
Dissertations, Master's Theses and Master's Reports - Open
We observed Santiaguito volcano in southwestern Guatemala from March 2008 - March 2010. Seismic and infrasound data collected between January and March of 2009 contain records of many diverse processes occurring at the dacitic dome complex, including the recurrence of short lived (30-200 seconds in duration) harmonic tremor concurrent with ash poor gas emissions from the volcano. We employ several different analytical techniques to examine different portions of the tremor and source mechanisms. We use the parameters derived by this analysis to compare the feasibility of several suggested models of eruption mechanisms, and determine that this type of harmonic tremor …
Sonic Log Prediction In Carbonates ,
2011
Michigan Technological University
Sonic Log Prediction In Carbonates , Nayyer Islam
Dissertations, Master's Theses and Master's Reports - Open
This work is conducted to study the complications associated with the sonic log prediction in carbonate logs and to investigate the possible solutions to accurately predict the sonic logs in Traverse Limestone. Well logs from fifty different wells were analyzed to define the mineralogy of the Traverse Limestone by using conventional 4-mineral and 3-mineral identification approaches. We modified the conventional 3-mineral identification approach (that completely neglects the gamma ray response) to correct the shale effects on the basis of gamma ray log before employing the 3-mineral identification. This modification helped to get the meaningful insight of the data when a …
