Fluid flow is a first-order feature of the geodynamic evolution of basins
as fault zones, strongly influence the mechanical behavior of the crust at different space and time scales (e.g., variations of fluid (over)pressure, seismogenic ...
Fluid flow is a first-order feature of the geodynamic evolution of basins and orogens. Fluids interact with rocks from the earliest stages of sedimentation until the stages these rocks are deformed and/or metamorphized and then exhumed. Fluids are major contributors to mineralization and ore deposits, hence of resources, and the interactions between fluid flows and tectonic structures, such as fault zones, strongly influence the mechanical behavior of the crust at different space and time scales (e.g., variations of fluid (over)pressure, seismogenic behavior). This session aims at making the point on our knowledge of fluid-rock-tectonics interactions in basins and forelands (deformed or not deformed) and at evaluating to what extent fluids influence, and in turn are influenced by, rock composition and physical/rheological properties and structural evolution (folds, fault zones) at different levels of the continental crust. We will focus on regional/case studies (e.g., fluid-rock interactions and fluid signatures in compressional, strike-slip or extensional settings) as well as on more technical aspects (recent advances in methods and techniques for fluid characterization and fluid pathways reconstruction, fluid-rock interaction modeling : geochemical transport-reactive; fluid-flow, mechanics, thermal and diagenesis modeling, dating of fluid circulation). We welcome contributions dealing with either hydrocarbon fluids (petroleum and gas systems; basin modeling) or hydrothermal and/or basinal fluids (mineralizing fluid systems). We also welcome works on the role and behavior of fracture systems and fault zones during fluid circulation in the crust down to the brittle-ductile transition (e.g., transient vs long-term fluid-rock interactions in fractures and faults, rock alteration related to fluid flow through faults, mineralizations and ore bodies associated with faults).
the automatic definition of fracture clusters (see Bellahsen et al., 2006a ..... plays an irregular shape, dissolution of the first cementa- tion phase before or during ...
compiled together on this histogram. (d) Comparison with histogram of distribution of homogenization temperature measured in pri- mary fluid inclusions in vein ...
6.3, and apply Newton's second law of motion. Where ..... Had water mixed with sawdust flow ..... In the course of this, the attack angles probably exceeded their.
still broadly debated and remains a key question to ... historical and present tectonic interactions. The ... Philippine Sea Plate and Australian Plate relative to the Eurasia Plate (De Mets et al., 1990; Seno et al., 1993). ..... solutions. The data
Contrary to classical basin simulators, this calculator does not require a ... INTRODUCTION ..... time subinterval where the grid definition deduced from ... describes an innovative technique designed to handle ... evolution. We use a formulation of
the characteristics of the grids introduced previously in the context of basin ...... tion of sand and pounce powder on a silicone basement in a 25 9 70 cm box (Fig.
whenever two layers slide over each other. This characteristic is called ..... since the cubic dilatation of the fluid is AV/V, the bulk modulus K is expressed by the ...
Department of Cell Biology, Duke University Medical Center, Durham,. NC 27710-3709. E-mail: .... Page 3 ... notes that arginine, lysine, phenylalanine, tyrosine and histidine ... (or whatever was the earliest cellular life form) and was passed.
environmental conditions. Recent genome-wide assess- ments of ... International Meeting of the Cassava Biotechnology Network,. Cali, Colombia, 8â14 March, ...
The phenomenon we consider here is the relatively well-known `Ternus ... The Ternus effect involves a multi-element stimulus that can lead to either of ... In the following section of this paper we consider mainly explanations that attempt ... elemen
ing of what really happens when introducing ICT into schools. Teaching and ... classroom use of technology became more practical, and literature matured, ..... contextual character of the meaning that students can develop when using ICT.
extensional stress could be more easily trans- mitted from ... jected to a stress regime which is controlled by local body ...... Giornale di Geologia, 48/1-2, 25-40.
the beneficiary of your life insurance policy! Larry, Mike and I all .... wind, after you compare airspeed to ... comparison, this is 16.9% less than the wet- ted area of ...
J1y o y . Introducing these expansions in Eq. 16 leads to the follow- ing quadratic equation: J1. 2. 1. S. J1. 1. S. F 00. This equation admits two real solutions only ...
Keywords: Fluid motion, optical flow, continuity equation, div-curl ..... the estimated divergence and the curl of the flow field is imposed through the quadratic.
aimed at stabilizing fixed points of the Navier-Stokes equations, such as those existing ..... where R is a weight matrix appearing in the chosen quadratic form.
Flow control is concerned with the targeted manipulation of intrinsic flow behavior to .... the flow, for example the signal from a wall-shear stress sensor. The.
Dec 21, 2013 - the LPS history, however, overpressure level can be defined by a mean gradient. .... southern part of the fold, the whole Paleozoic sedimentary suc- ..... that syn-folding fractures caused a high vertical hydraulic perme- ... compare f
Up to this point the equations governing fluid flow and solid mechanics appear to be similar with ... each of which has a certain behaviour in the numerical solution. ..... To complete the relationship it is necessary to determine heat source terms.
Kelif, Fluid Model of Wireless Networks, Thesis, ENST Telecom Paris, France, Feb 2008. [17] M. Kalantari, M. Shayman, Routing in wireless ad hoc networks by ...
shown to produce tractable, closed-form formulas: Poisson networks (the interfering Base Stations (BSs) locations form a Poisson process) and fluid networks ...
cussion nor his figure is sufficiently detailed to construct a ... Diatropornis differs from most other cathartids in having the .... REMARKS: Gaillard (1908) described A. schlosseri ..... Miller, who devoted much of his scientific career to the stud
weaken the crust, down to the strength of the inherited faults. .... was disharmonically folded over these shear zones (Bellahsen et al., ..... for theoretical RXY.
