Big Chemical Encyclopedia

Chemical substances, components, reactions, process design ...

Articles Figures Tables About

Orogenic mechanism

Protein-LMWE Mixed Films (Orogenic Mechanism).270... [Pg.251]

Recent works by the Norwich group (Gunning et al., 1999 Mackie et ak, 1999, 2000 Wilde, 2000) have demonstrated how surfactants disrupt and displace proteins from an interface by a three-stage "orogenic" mechanism. We have adopted this mechanism to describe spread protein-LMWE mixed films (Figure 14.8) (Patino et al., 2003). The results suggest that for spread... [Pg.270]

Three-stage "orogenic" mechanism for displacement of proteins by water-insoluble LMWE spread at the air-water interface. [Pg.270]

Bodinier, J. L., Vasseur, G., Vernieres, J., Dupuy., C. Fabries, J. (1990). Mechanisms of mantle metasomatism Geochemical evidence from the Lherz orogenic peridotite. J. [Pg.527]

Even though paleoaltimetric data from internal structural elements of orogenic belts and plateaus represent much needed complementary information to those derived from surface deposits or weathering products we caution about the uncritical use of stable isotopic data from deeper Earth environments in paleoaltimetric studies. It is highly desirable to obtain reliable thermometric, structural, and isotopic tracer data before attempting any paleoaltimetric reconstruction in such environments, as uncertainties exist about the fluid pathways and mechanisms responsible for fluid transport into the ductile crust. Maybe more importantly, it is imperative to document that the timing of meteoric water-rock interaction can be dated precisely, especially within thermally and kinematically rapidly evolving tectonic environments such as extensional detachment systems. [Pg.110]

Willett S., Beaumont C., and Fullsack P. (1993) Mechanical model for the tectonics of doubly vergent compressional orogens. Geology 21, 371-374. [Pg.1554]

Pressley R. A. and Brown M. (1999) The Phillips pluton, Maine, USA evidence of heterogeneous crustal sources and implications for granite ascent and emplacement mechanisms in convergent orogens. Uthos 46, 335—366. [Pg.1670]

The orogenic displacement mechanism is a consequence of the low level of interaction between proteins and LMWE at the air-water interface. This model has been shown to work for a range of proteins with different secondary and tertiary structures and different t)q)es of LMWE (monoglycerides and phospholipids). [Pg.271]


See other pages where Orogenic mechanism is mentioned: [Pg.329]    [Pg.331]    [Pg.331]    [Pg.271]    [Pg.280]    [Pg.282]    [Pg.329]    [Pg.331]    [Pg.331]    [Pg.271]    [Pg.280]    [Pg.282]    [Pg.1]    [Pg.2]    [Pg.14]    [Pg.92]    [Pg.92]    [Pg.92]    [Pg.102]    [Pg.108]    [Pg.113]    [Pg.293]    [Pg.806]    [Pg.810]    [Pg.811]    [Pg.828]    [Pg.844]    [Pg.845]    [Pg.858]    [Pg.858]    [Pg.1338]    [Pg.1530]    [Pg.1539]    [Pg.1574]    [Pg.1663]    [Pg.2214]    [Pg.278]    [Pg.104]    [Pg.108]    [Pg.109]    [Pg.126]    [Pg.142]    [Pg.143]    [Pg.156]    [Pg.156]   
See also in sourсe #XX -- [ Pg.270 , Pg.284 ]




SEARCH



Orogenic displacement mechanism

© 2024 chempedia.info