Ord Alison (33 results)

Softcover/Paperback. Condition: Sehr gut. P. 338 - 487 : ill. ; 24 cm. Sehr guter Zustand. Minimale Lager- bzw. Gebrauchsspuren. / Very good. Minimal wear. Sprache: Englisch Gewicht in Gramm: 390.

Condition: New. This is a Brand-new US Edition. This Item may be shipped from US or any other country as we have multiple locations worldwide.

Condition: Used. pp. 248.

Condition: Used. pp. 248 Illus.

Hardcover. Condition: New. Brand new book, sourced directly from publisher. Dispatch time is 9-10 days from our warehouse. Book will be sent in robust, secure packaging to ensure it reaches you securely.

hardcover. Condition: Good. Connecting readers with great books since 1972! Used textbooks may not include companion materials such as access codes, etc. May have some wear or writing/highlighting. We ship orders daily and Customer Service is our top priority.

Condition: Used. pp. 248.

Condition: Brand New. New. US edition. Expediting shipping for all USA and Europe orders excluding PO Box. Excellent Customer Service.

Condition: As New. Unread book in perfect condition.

Condition: new. New.

Condition: New.

Condition: New.

Condition: New. In English.

Condition: As New. Unread book in perfect condition.

Hardback. Condition: New. 2008 ed. The study of heat transfer mechanisms in hydrothermal systems is important for understanding the basic physics behind orebody formation and mineralization in the upper crust (Bickle and Mckenzie 1987; Bjorlykke et al. 1988; Brady 1988; England and Thompson 1989; Hoisch 1991; Connolly 1997). Generally, heat energy may be transferred within the crust in the following forms: conduction, advection (including forced convection) where the heat is carried by a moving mass of rock during def- mation or by a moving uid, convection (i. e. , free convection, natural convection, buoyancy driven convection, temperature gradient driven convection) and a com- nation of these processes. Since advective ow is usually generated by a pore- uid pressure gradient, heat transfer due to advective ow is largely dependent on the pore- uid pressure gradient distribution in hydrothermal systems. A typical ex- ple of this advective ow is the upward through ow caused by lithostatic pore- uid pressure gradients within the lower crust. Extensive studies (Connolly and Ko 1995; Etheridge et al. 1983; England et al. 1987; Fyfe et al.1978; Walther and Orville 1982; Peacock 1989; Yardley and Bottrell 1992; Hanson 1992; Yardley and Lloyd 1995; Norton and Knapp 1970) have shown that lithostatic pore- uid pressure can be built up by metamorphic uids arising from devolatilization and dehydration - actions, if the permeability is low enough to control uid ow in the lower crust. …

Hardcover. Condition: Brand New. 1st edition. 680 pages. 9.25x7.50x1.50 inches. In Stock.

Condition: New. pp. xvi + 230.

Condition: New. In English.

Hardcover. Condition: Brand New. 1st edition. 230 pages. 9.50x6.25x0.75 inches. In Stock.

Paperback. Condition: Brand New. 246 pages. 9.00x6.00x0.59 inches. In Stock.

Condition: New.

Condition: New. In English.

Condition: New. pp. 260.

Softcover. Condition: gut. Localization of deformation in rocks and metals. In deutscher Sprache. pages.

Hardback. Condition: New. 2008 ed. The study of heat transfer mechanisms in hydrothermal systems is important for understanding the basic physics behind orebody formation and mineralization in the upper crust (Bickle and Mckenzie 1987; Bjorlykke et al. 1988; Brady 1988; England and Thompson 1989; Hoisch 1991; Connolly 1997). Generally, heat energy may be transferred within the crust in the following forms: conduction, advection (including forced convection) where the heat is carried by a moving mass of rock during def- mation or by a moving uid, convection (i. e. , free convection, natural convection, buoyancy driven convection, temperature gradient driven convection) and a com- nation of these processes. Since advective ow is usually generated by a pore- uid pressure gradient, heat transfer due to advective ow is largely dependent on the pore- uid pressure gradient distribution in hydrothermal systems. A typical ex- ple of this advective ow is the upward through ow caused by lithostatic pore- uid pressure gradients within the lower crust. Extensive studies (Connolly and Ko 1995; Etheridge et al. 1983; England et al. 1987; Fyfe et al.1978; Walther and Orville 1982; Peacock 1989; Yardley and Bottrell 1992; Hanson 1992; Yardley and Lloyd 1995; Norton and Knapp 1970) have shown that lithostatic pore- uid pressure can be built up by metamorphic uids arising from devolatilization and dehydration - actions, if the permeability is low enough to control uid ow in the lower crust. …

Hardcover. Condition: Brand New. 1st edition. 323 pages. 9.75x6.50x0.50 inches. In Stock.

Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Derivation of analytical solutions to advanced problems involving fluid and thermal transport in rocks with associated benchmark solutionsDr Chongbin Zhao obtained BE and PhD in Tsinghua University, China. He worked as Postdoctoral Research Fe.…

Gebunden. Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Derivation of analytical solutions to advanced problems involving fluid and thermal transport in rocks with associated benchmark solutionsDr Chongbin Zhao obtained BE and PhD in Tsinghua University, China. He worked as Postdoctoral Research Fe.…

Condition: New. Print on Demand pp. xvi + 230 89 Illus. (9 col.).

Condition: New. PRINT ON DEMAND pp. xvi + 230.