منابع مشابه
Triassic Stratigraphy in the Zuni Mountains, West-central New Mexico
—The Triassic System in the Zuni Mountains consists of one Middle Triassic unit, the Moenkopi Formation, the Upper Triassic Chinle Group, and the Upper Triassic-Lower Jurassic(?) Wingate Sandstone. The Chinle Group in the Zuni Mountains consists of six formations, in ascending order: Zuni Mountains (named here; = “mottled strata” of previous workers), Shinarump, Bluewater Creek, Petrified Fores...
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Beginning with this issue, the Journal of Paleontology will be publishing an occasional section entitled ‘‘View from the Field’’. ‘‘View from the Field’’ will provide a forum for concise commentary on current issues in paleontology, including but not limited to discussion of methods, important new discoveries, and major conceptual advances. Contributions should be brief (no more than 12 double-...
متن کاملSequence Stratigraphy
Sequence stratigraphy is the study of sediments and sedimentary rocks in terms of repetitively arranged facies and associated stratal geometry (Vail 1987; Van Wagoner et al 1988, 1990; Christie-Blick 1991). It is a technique that can be traced back to the work of Sloss et al (1949), Sloss (1950, 1963), and Wheeler (1958) on interregional unconformities of the North American craton, but it becam...
متن کاملMESH r-ADAPTATION FOR UNILATERAL CONTACT PROBLEMS†
The aim of this paper is to present an algorithm of topology preserving mesh adaptation. It is based on a node movement rather than on mesh classical refinement/coarsening techniques. The choice of this so-called r-adaptation strategy is motivated at least by two reasons: node movement techniques preserve the matrix structure and are then well suited for large-scale computations, e.g. three-dim...
متن کاملFictitious Domain Formulation of Unilateral Problems
The fictitious domain method for the solution of variational inequalities with the Signorini boundary conditions is analyzed.
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ژورنال
عنوان ژورنال: ESAIM: Mathematical Modelling and Numerical Analysis
سال: 2006
ISSN: 0764-583X,1290-3841
DOI: 10.1051/m2an:2006029