Thrust Tectonics and Hydrocarbon Systems
Thrust Tectonics and Hydrocarbon Systems resulted from an international conference at Royal Holloway University in London. The volume contains 33 chapters divided into four sections:Geodynamics of Thrust Systems, Analog Modeling of Thrust Systems, Fault-Related Folds in Thrust Systems,and Case Studies. These papers summarize recent advances in thrust studies and their application to hydrocarbon exploration and production.Key topics addressed include the application of the critically tapered Coulomb wedge model to thrust systems both in nature and in experiments, the interaction of surface proceses with thrust systems, basement-involved thrust systems and inversion, fault-related folds in thrust belts, and growth stratal development in thrust belts. Fold-and thrust belts described and discussed in this volume include the Alps, the Andes, the Apennines, the Appalacians, the Alice Springs Orogen in Australia, the Albanides, the Atlas in Morocco, the Canadian Cordillera and the Canadian Rocky Mountains, Kutei Basin, Kalimantan, the Himalayas, the New England Orogen, Papua New Guinea, and the Spanish Pyrenees, as well as depwater fold and thrust belts such as the Niger Delta and the Gulf of Mexico. Memoir 82 provides an in-depth look at thrust tectonics and hydrocarbon systems, and is a milestone publication as a major new examination of thrust fault systems.
Thrust Tectonics and Hydrocarbon Systems; Introduction
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Published:January 01, 2004
The tectonic settings and internal characteristics of fold-and-thrust belts are remarkably varied and diverse. They include
classic thin-skinned Canadian Rocky Mountain-style foreland fold-and-thrust belts (Bally et al., 1966; Price, 1981; Barclay and Smith, 1992);
basement-involved Laramide uplifts of the western U.S.A. (Schmidt et al., 1993);
subduction-related thrust systems of the Andes (Ramos et al., 2004 [this volume]), the Zagros (Beydoun et al., 1992), and Papua New Guinea (Cole et al., 2000; Hill et al., 2000; and Hill et al., 2004 [this volume]);
collision terranes of the Himalayas (e.g., Mugnier et al., 2004 [this volume]), and the Italian Apennines (Coward et al., 1999; Turrini and Rennison, 2004 [this volume]); and
deep-water, gravitationally driven fold-and-thrust belts, such as those offshore West Africa or in the Gulf of Mexico (Rowan et al., 2004 [this volume]).
Many of these fold-and-thrust belts contain major hydrocarbon accumulations in complex structural traps. Hydrocarbon exploration in many onshore fold-and-thrust belts commonly is very difficult because of rugged and severe terrain, complex structures, and poor-quality seismic data.
Key to understanding the 4-D evolution of fold-and-thrust-belt systems are an appreciation of the driving mechanisms for thrust-belt development, and knowledge of the timing of thrust movements, their burial and thermal evolution, and their uplift and exhumation histories. Understanding both the spatial and temporal evolution of fold-and-thrust belts is vital for viable hydrocarbon exploration and development in these complex terranes. This volume presents key papers that address current issues in understanding fold-and-thrust-belt structures. These include (1) fold-and-thrust-belt geodynamics, (2) 3-D thrust geometries, (3) scaled analog modeling of thrust belts as a means of developing new kinematic models for their evolution, (4) new models of thrust-fault-related folds and synkin-ematic growth strata, and (5) case studies of particular thrust terranes.
Several key topics are addressed in this volume.