Results 241 to 250 of about 714,372 (264)

Thermal Structure of the Anadarko Basin

AAPG Bulletin, 1999
The Anadarko basin of Oklahoma is a two-stage Paleozoic cratonic basin with as much as 12 km (7.5 mi) or more of sedimentary fill. We present a present-day thermal model of the basin based on lithologic analysis at 3-m (10-ft) intervals in 63 wells, heat flow measurements at seven sites, and in-situ thermal conductivity calibration of the sediment ...
David D. Blackwell, Jaquidon D. Gallardo
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Structure of Mono Basin, California

Journal of Geophysical Research, 1970
In a recent paper, Christensen et al. [1969] interpreted the gravity and seismic data from Mono Basin, California, to indicate that the depth to the basement there is 1–1.5 km, whereas Pakiser et al. [1960] and Pakiser [1968] interpreted the same data to indicate a depth of 5–5.5 km, with an acknowledged uncertainty of 1–1.5 km. Christensen et al. were
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Venezuela Basin crustal structure

Journal of Geophysical Research: Solid Earth, 1981
Velocity‐depth profiles derived from six two‐ship expanding spread experiments, in combination with other geophysical data, define the characteristics of two distinct types of Venezuela Basin crust and the boundary between them. Each two‐ship common midpoint reflection/refraction profile is automatically transformed into the τ‐p plane, ‘picked’ and ...
John B. Diebold, Paul L. Stoffa, Peter Buhl, Marek Truchan   +3 more
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The structure of the Dead Sea basin

Tectonophysics, 1996
Abstract The Dead Sea basin is located along the left-lateral transform boundary between the Arabian and Sinai plates. Its structure and history are known from surface geology, drilling, seismic reflection and other geophysical data. The basin comprises a large pull-apart, almost 150 km long and mostly 8–10 km wide, which is flanked by a few ...
Zvi Ben-Avraham, Zvi Garfunkel
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Application of Magnetics to Basin Structures

Proceedings, 1995
Magnetic surveys have long been part of basin exploration but the use has either been for reconnaissance purposes, basement depth estimates, general mapping applications or some detailed review of isolated features. The data have been generally underutilised.
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The structure of the South Fiji basin

Tectonophysics, 1982
Abstract New magnetic, seismic and bathymetric data show that the South Fiji basin is a structurally complex marginal basin. A gap in the identifiable magnetic anomaly lineations exist over the central part of the basin and prevents the unequivocal linking of the anomaly lineations (anomalies 7A to 12) associated with the ridgc-ridge-ridge triple ...
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The structure of basins of attraction and their trapping regions

Ergodic Theory and Dynamical Systems, 1997
In dynamical systems examples are common in which two or more attractors coexist, and in such cases, the basin boundary is nonempty. When there are three basins of attraction, is it possible that every boundary point of one basin is on the boundary of the two remaining basins? Is it possible that all three boundaries of these basins coincide? When this
Helena E. Nusse, James A. Yorke
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Origin and structure of the Basin ranges

Geological Society of America Bulletin, 1901
Introduction Investigation of the structure of the desert ranges which lie between the Wasatch and the Sierra and extend southward into California is no easy task. In the past different views have been held, some seeing in them a series of parallel folds in which the anticlines protruding above the surface formed the ranges, while others considered ...
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THE STRUCTURAL FEATURES OF XISHA TROUGH BASIN

Marine Geology & Quaternary Geology, 2013
The Xisha Trough Basin,located on the continental slope of the northern South China Sea,is a Cenozoic deepwater basin.The sediment fill in the basin is about 1500 ~ 8000m in thickness,and becomes thinner from the center towards north and south.The sediments show a zonal distribution pattern in north-south direction.In seismic profiles,there is double ...
Guangjian Zhong, Changmao Feng, Zhenquan Wei   +2 more
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The structural development of the Wessex Basin

Journal of the Geological Society, 1982
The Mesozoic and Cenozoic structures of southern England form part of a system of disturbances which extends across the Channel into northern France. They are reviewed in the light of published data from south Dorset. Basin development started with Permo-Triassic rifting, and is believed to have continued through the Jurassic and early Cretaceous with ...
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