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sediments
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
physiographic provinces
A “natural sand plant” at the shelf edge in the low-energy Gulf of Lions, western Mediterranean Sea Available to Purchase
Limited Evidence of Late Quaternary Tectonic Surface Deformation in the Eastern Tennessee Seismic Zone, United States Available to Purchase
Storm-driven sedimentation and dynamics of a sediment slug in an ephemeral stream: Influence on sediment-routing systems within source areas Open Access
First-order CO 2 trapping characteristics of fold-and-thrust belts: Assessing carbon storage potential in the Appalachian Basin and beyond Available to Purchase
Eroding the Himalaya: Topographic and Climatic Control of Erosion Rates and Implications for Tectonics Available to Purchase
PHYSIOGRAPHIC LANDFORM CARTOGRAPHY: A COMPARATIVE ANALYSIS OF CONTRIBUTIONS BY ARMIN K. LOBECK (1921) AND ERWIN RAISZ (1939) Available to Purchase
Pliocene Drainage in Manitoba and Northwestern Ontario, Canada Available to Purchase
Sub-watershed Prioritization Based on Drainage Morphometric Analysis: A Case Study of Cauvery River Basin in South India Available to Purchase
Stromatolite Provinces of Hamelin Pool: Physiographic Controls On Stromatolites and Associated Lithofacies Available to Purchase
Assessment of Interactions between River and Aquifer in the Gowri-hole Sub-catchment Available to Purchase
High‐Resolution 2D Lg and Pg Attenuation Models in the Basin and Range Region with Implications for Frequency‐Dependent Q Available to Purchase
Effects of sedimentary facies on structural styles in the Canadian Rocky Mountain Fold and Thrust Belt Available to Purchase
ABSTRACT The Rocky Mountain Fold and Thrust Belt west of Calgary, Alberta, has a long history of surface geologic mapping and hydrocarbon exploration. Many of these data are in the public domain. As a consequence of this excellent data set, the stratigraphy, sedimentology, and structural geology are very well understood. Major stratigraphic boundaries or facies transitions within Paleozoic units control structural detachment levels, the mechanical behavior of these lithotectonic units, and the structural styles observed. Fault terminations such as lateral ramps and relay zones often occur within depositional fairways comprised of less competent strata. The major facies transition near Field, British Columbia, and the resulting contrast in structural styles between the Eastern Main Ranges and Western Main Ranges will be observed. Two dip transects across the belt will document the foreland progression of major thrust faults or fault systems, and attempt to tie the age of these faults to the timing of terrane accretion and deformation events observed to the west within the southern Canadian Cordillera.
Anatomy And Sequence Architecture of the Early Post-Rift In the Neuquén Basin (Argentina): A Response To Physiography and Relative Sea-Level Changes Available to Purchase
Sulfur Isotopes in Plutonic Rocks of the Great Basin as Indicators of Crustal Architecture Available to Purchase
Physiographic provinces of the Arctic Ocean seafloor Available to Purchase
Structural Geology of the Colorado Plateau Region of Southern Utah, with Special Emphasis on Deformation Bands
Abstract This wide-ranging discussion of Precambrian rocks includes contributions from a diverse array of authors actively engaged in investigations of various aspects of U.S. Precambrian geology. Summary discussions by the editors of the five major chapters place these contributions in a logical regional framework. A concluding chapter explores Archean crustal processes from the point of view of lunar and planetary analogies, discusses the significance of Sm crustal provinces, and provides an overview of the development of the southern parts of Laurentia. Accompanying plates include a newly compiled map of the Precambrian rocks of the conterminous U.S., maps showing relationships of the Precambrian geology to magnetic anomalies and to isostatic residual gravity, and a new correlation chart for U.S. Precambrian rocks.
Abstract DNAG Transect H-1. Part of GSA’s DNAG Continent-Ocean Transect Series, this transect contains all or most of the following: free-air gravity and magnetic anomaly profiles, heat flow measurements, geologic cross section with no vertical exaggeration, multi-channel seismic reflection profiles, tectonic kindred cross section with vertical exaggeration, geologic map, stratigraphic diagram, and an index map. All transects are on a scale of 1:500,000.