High-Resolution Approaches in Stratigraphic Paleontology
High-Resolution Approaches in Stratigraphic Paleontology

Author: P.J. Harries

Publisher: Springer Science & Business Media

Published: 2008-07-30

Total Pages: 480

ISBN-13: 1402090536

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This volume delves into a spectrum of theoretical as well as applied aspects of high-resolution stratigraphic approaches in paleontology. It explores how increasingly detailed knowledge of the fossil record can enhance our understanding of the evolution of life on Earth and also allows geoscientists to address a broad range of important evolutionary and environmental questions in this arena. A 'zipped' version of the program CONOP9 2007 along with read-me files, sample files, and other documentation are available via a web site (see below). An earlier version of CONOP9 was initially supplied with 'High-Resolution Approaches in Stratigraphic Paleontology' (PJ Harries, editor) and described in Chapter 13 of that volume. This is an updated version of the program, and the documentation supplied with this version supersedes the information supplied in that chapter. To view the CONOP9 Programs, click on the link CONOP9 Programs on the right side of this page under Related links.

Lacustrine Sandstone Reservoirs and Hydrocarbon Systems
Lacustrine Sandstone Reservoirs and Hydrocarbon Systems

Author: Olive W. Baganz

Publisher: AAPG

Published: 2012-11-20

Total Pages: 526

ISBN-13: 0891813772

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Many publications on lacustrine systems concentrate on reconstructing paleo-environments, deciphering paleoclimate or estimating hydrocarbon source potential. This is the first memoir to give attention to describing the occurrence, distribution and character of sandstones in various lake settings. The memoir is divided into four sections beginning with a global overview, and followed by two sections covering lacustrine systems in compressional and extensional regimes, and concludes with a series of papers on modern lake regimes.

Investigation of land subsidence and earth fissures in Cedar Valley, Iron County, Utah
Investigation of land subsidence and earth fissures in Cedar Valley, Iron County, Utah

Author: Paul Inkenbrandt

Publisher: Utah Geological Survey

Published: 2014-03-12

Total Pages: 122

ISBN-13: 1557918910

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This 116-page report presents the results of an investigation by the Utah Geological Survey of land subsidence and earth fissures in Cedar Valley, Iron County, Utah. Basin-fill sediments of the Cedar Valley Aquifer contain a high percentage of fine-grained material susceptible to compaction upon dewatering. Groundwater discharge in excess of recharge (groundwater mining) has lowered the potentiometric surface in Cedar Valley as much as 114 feet since 1939. Groundwater mining has caused permanent compaction of fine-grained sediments of the Cedar Valley aquifer, which has caused the land surface to subside, and a minimum of 8.3 miles of earth fissures to form. Recently acquired interferometric synthetic aperture radar imagery shows that land subsidence has affected approximately 100 mi² in Cedar Valley, but a lack of accurate historical benchmark elevation data over much of the valley prevents its detailed quantification. Continued groundwater mining and resultant subsidence will likely cause existing fissures to lengthen and new fissures to form which may eventually impact developed areas in Cedar Valley. This report also includes possible aquifer management options to help mitigate subsidence and fissure formation, and recommended guidelines for conducting subsidence-related hazard investigations prior to development.

Geology of the Sulphurdale geothermal-resource area, Beaver and Millard Counties, Utah
Geology of the Sulphurdale geothermal-resource area, Beaver and Millard Counties, Utah

Author: P.D. Rowley

Publisher: Utah Geological Survey

Published: 2013-04-15

Total Pages: 33

ISBN-13:

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This 27-page report analyzes new detailed (1:12,000 scale) geologic mapping of a 14 square mile area centered by the high-temperature (350°F) Sulphurdale heat source, which at the surface makes up a circular area about a mile in diameter that is likely caused by a magma body at depth. A former small steam-driven geothermal electric power plant in the circular area is being replaced by a larger plant (Enel Green Power North America) that will use binary technology. Five cross sections tied to and at the same scale as the map help interpret the likely extent of the geothermal resource. Sulfur derived from evaporites at depth was initially mined at a solfatara above the heat source; associated sulfuric acid seeped downward to remove the Kaibab Limestone and Toroweap Formation from the subsurface.

Accommodation zones and transfer zones; the regional segmentation of the Basin and Range Province
Accommodation zones and transfer zones; the regional segmentation of the Basin and Range Province

Author: James E. Faulds

Publisher: Geological Society of America

Published: 1998-01-01

Total Pages: 269

ISBN-13: 081372323X

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This volume focuses on the geometry, kinematic development, and origin of regional segmentation structures within the basin and range province of Western North America. Contributions range from analysis of individiual structures to broad regional syntheses, including a map of basin and range structures and tilt domains. Several papers discuss the implications of regional segmentation structures in assessing seismic hazards, hydrocarbon and mineral resources, and ground-water supplies.

The Gigantic Markagunt and Sevier Gravity Slides Resulting from ­ Mid-Cenozoic Catastrophic Mega-Scale Failure of the Marysvale Volcanic Field, Utah, USA
The Gigantic Markagunt and Sevier Gravity Slides Resulting from ­ Mid-Cenozoic Catastrophic Mega-Scale Failure of the Marysvale Volcanic Field, Utah, USA

Author: Robert F. Biek

Publisher: Geological Society of America

Published: 2019-12-31

Total Pages: 132

ISBN-13: 0813700566

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"The Markagunt and Sevier gravity slides are gigantic landslides that resulted from gravitationally induced catastrophic failure of the southern flank of the Oligocene to Miocene Marysvale volcanic field. Each is nearly 100 km long with runouts over the former land surface>35 km; together they span 7000 km2 and rank among Earth's largest terrestrial landslides. Basal cataclastic layers, injectites, pseudotachylyte, deformed clasts, and a variety of kinematic indicators demonstrate catastrophic emplacement, which was preceded by slow gravitational spreading of the volcanic field. This volume offers a history of their discovery, our current understanding of the gravity slides, and a guide to particularly instructive exposures for which the authors document their conclusions about the size, age, and significant structural features of these newly discovered features"--