Passchier cees (43 résultats)

Paperback. Etat : Gut. 72 p., with numerous figures, 28 cm, Cover faded, otherwise good condition. Note of ownership. Sprache: Englisch Gewicht in Gramm: 400.

Etat : New.

Paperback or Softback. Etat : New. Field Geology of High-Grade Gneiss Terrains. Book.

Etat : New.

Etat : As New. Unread book in perfect condition.

Perfect Paperback. Etat : New.

Etat : New.

Etat : New. In English.

Groß-8°, paperback edition. Etat : Gut. 150 pages, text in English, black and white photos, graphic representations, contents, problem section, introduction, informative misinterpretation, references, index, illustrated cover Passchier et al.: Field Geology of High-Grade Gneiss Terrains. This is the textbook on structural geology aimed primarily at the interpretation of high-grade gneiss terrains. The autors outline some of the more commonly seen structural features, suggest how they can be analysed and interpreted, and explain which sampling technique for petrology, geochemistry and geochronologie will give the best results. The text is lavishly illustrated with line drawings and photographes, and features chapters on "Mapping in Gneiss Terrains", "Fabric Development", "Interpretation of Structures and Fabrics", Metamorphic History of Gneiss Terrains", "Geochemistry, Isotope geochemistry and Geochronology" and "Origin and Evolution of High-Gnade Gneiss Terrains", A "Problem Section" includes illustrated examples of structures that are difficult to interpret and which allow readers to test their skills. Sprache: Englisch Gewicht in Gramm: 340.…

Etat : As New. Unread book in perfect condition.

Perfect Paperback. Etat : Brand New. 1st edition. 159 pages. 9.53x6.69x0.37 inches. In Stock.

Etat : New.

perfect. Etat : New. In shrink wrap. Looks like an interesting title.

Hardcover. Etat : New. In shrink wrap. Looks like an interesting title.

Paperback. Etat : Very Good. The book has been read, but is in excellent condition. Pages are intact and not marred by notes or highlighting. The spine remains undamaged.

Etat : New. pp. 366.

Taschenbuch. Etat : Neu. Microtectonics | Cees W. Passchier (u. a.) | Taschenbuch | xvi | Englisch | 2014 | Springer | EAN 9783642441110 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu.

Paperback. Etat : Brand New. 2nd edition. 384 pages. 10.00x7.50x1.00 inches. In Stock.

Paperback. Etat : Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Etat : New.

Etat : New. In English.

Etat : gut. 1991. Shear-sense Indicators: A Review (=Geological Survey of Canada, Paper 90-17).) In englischer Sprache. pages.

Etat : New. pp. 329.

Etat : New. PP. viii + 322.

Paperback. Etat : Brand New. reprint edition. 322 pages. 10.98x8.26x0.69 inches. In Stock.

Paperback. Etat : Like New. LIKE NEW. SHIPS FROM MULTIPLE LOCATIONS. book.

Etat : As New. Unread book in perfect condition.

Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field. 164 pp. Englisch.…

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

Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under went, can usually best be determined by straightforward observation in the field.Springer-Verlag KG, Sachsenplatz 4-6, 1201 Wien 164 pp. Englisch.…