Amadei B (14 results)

Hardcover. Condition: Fine. 1st Edition. (Mining - Engineering) ROCK MECHANICS FOR INDUSTRY / Proceedings Of The 37th U.S. Rock Mechanics Symposium, Vail, Colorado, USA, 6-9 June 1999. Edited by Bernard Amadei etal. Two volumes, A. A. Balkema, Rotterdam,Brookfield, 1999. Large 8vo size books, green clth bindings plastic coated and illustrated, both bindings in extra fine condition. Together 1250-pages of text, fine throughout; drawings, charts, some illustration.…

Brossura. Condition: ottimo. prima edizione. Catalogo mostra, Alba, Ottobre- Novembre 2003Num Pagine 98. Illustrazioni a colori e in bianco e nero fuori testo. colori e b/n (illustrator).

Condition: new.

Hardcover. Condition: Brand New. 1st edition. 1278 pages. 9.75x7.00x1.50 inches. In Stock.

Condition: Gut. Zustand: Gut | Seiten: 512 | Sprache: Englisch | Produktart: Bücher | Rock masses are initially stressed in their current in situ state of stress and to a lesser natural state. Whether one is interested in the extent on the monitoring of stress change. formation of geological structures (folds, faults, The subject of paleostresses is only briefly intrusions, etc. ), the stability of artificial struc­ discussed. tures (tunnels, caverns, mines, surface excava­ The last 30 years have seen a major advance our knowledge and understanding of rock tions, etc. ), or the stability of boreholes, a in the in situ or virgin stress field, stress. A large body of data is now available on knowledge of along with other rock mass properties, is the state of stress in the near surface of the needed in order to predict the response of rock Earth's crust (upper 3-4km of the crust). masses to the disturbance associated with those Various theories have been proposed regarding structures. Stress in rock is usually described the origin of in situ stresses and how gravity, within the context of continuum mechanics. It is tectonics, erosion, lateral straining, rock fabric, defined at a point and is represented by a glaciation and deglaciation, topography, curva­ second-order Cartesian tensor with six compo­ ture of the Earth and other active geological nents. Because of its definition, rock stress is an features and processes contribute to the current enigmatic and fictitious quantity creating chal­ in situ stress field.…

Condition: Sehr gut. Zustand: Sehr gut | Seiten: 512 | Sprache: Englisch | Produktart: Bücher | Rock masses are initially stressed in their current in situ state of stress and to a lesser natural state. Whether one is interested in the extent on the monitoring of stress change. formation of geological structures (folds, faults, The subject of paleostresses is only briefly intrusions, etc. ), the stability of artificial struc­ discussed. tures (tunnels, caverns, mines, surface excava­ The last 30 years have seen a major advance our knowledge and understanding of rock tions, etc. ), or the stability of boreholes, a in the in situ or virgin stress field, stress. A large body of data is now available on knowledge of along with other rock mass properties, is the state of stress in the near surface of the needed in order to predict the response of rock Earth's crust (upper 3-4km of the crust). masses to the disturbance associated with those Various theories have been proposed regarding structures. Stress in rock is usually described the origin of in situ stresses and how gravity, within the context of continuum mechanics. It is tectonics, erosion, lateral straining, rock fabric, defined at a point and is represented by a glaciation and deglaciation, topography, curva­ second-order Cartesian tensor with six compo­ ture of the Earth and other active geological nents. Because of its definition, rock stress is an features and processes contribute to the current enigmatic and fictitious quantity creating chal­ in situ stress field.…

Condition: New. In English.

Condition: New. In English.

Condition: New.

Condition: New. Unlike man made materials such as concrete and steel, natural materials such as rocks and soils are subject to natural (virgin) stresses called in-situ stresses. Many theories have been proposed regarding their origin and various techniques have been developed to measure in-situ stresses. This book deals with this topic. Num Pages: 490 pages, biography. BIC Classification: RBG; TNCC; TT. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly. Dimension: 266 x 188 x 34. Weight in Grams: 1140. . 1997. 1997th Edition. hardcover. . . . .…

Condition: New. Unlike man made materials such as concrete and steel, natural materials such as rocks and soils are subject to natural (virgin) stresses called in-situ stresses. Many theories have been proposed regarding their origin and various techniques have been developed to measure in-situ stresses. This book deals with this topic. Num Pages: 490 pages, biography. BIC Classification: RBG; TNCC; TT. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly. Dimension: 266 x 188 x 34. Weight in Grams: 1140. . 1997. 1997th Edition. hardcover. . . . . Books ship from the US and Ireland.…

Condition: new. Questo è un articolo print on demand.

Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Rock masses are initially stressed in their current in situ state of stress and to a lesser natural state. Whether one is interested in the extent on the monitoring of stress change. formation of geological structures (folds, faults, The subject of paleostr. …

Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Rock masses are initially stressed in their current in situ state of stress and to a lesser natural state. Whether one is interested in the extent on the monitoring of stress change. formation of geological structures (folds, faults, The subject of paleostr. …