Edward Sobel (6 results)

Condition: Good. Good condition. 1996. A copy that has been read but remains intact. May contain markings such as bookplates, stamps, limited notes and highlighting, or a few light stains. NOT AVAILABLE FOR SHIPMENT OUTSIDE OF THE UNITED STATES.

Hardcover. Condition: New.

Softcover, single sheet folded twice to form 3 panels printed both sides; good condition; moderate rubbing to cover; long crease to edge of all pages.

hardcover. Condition: Very Good. This hardcover copy is in very good condition. Its text is clean and unmarked, its binding is sound with no loose or missing pages, and it shows light signs of handling wear. The hinge is slightly cracked at the rear just before the rear free endpaper. More photos are available upon request. Tulsa's largest used bookstore. Located on South Mingo Road since 1991. No-hassle return policy if not completely satisfied.

Paperback. Condition: Brand New. 400 pages. 9.75x7.00x0.75 inches. In Stock.

Hardcover. Condition: New. The geological evolution of Central Asia commenced with the formation of a complex Precambrian-Palaeozoic orogen. Cimmerian blocks were then accreted to the southern margin in the Mesozoic, leading to tectonic reactivation of older structures and discrete episodes of basin formation. The Indian and Arabian blocks collided with Asia in the Cenozoic, leading to renewed structural reactivation, intracontinental deformation and basin development. This complex evolution resulted in the present-day setting of an elongated Tien Shan range flanked by large Mesozoic-Cenozoic sedimentary basins with smaller intramontane basins distributed within the range. This volume presents multidisciplinary results and reviews from research groups in Europe and Central Asia that focus on the western part of the Tien Shan and some of the adjacent large sedimentary basins. These works elucidate the Late Palaeozoic-Cenozoic tectono-sedimentary evolution of the area. Emphasis is given to the collision of terranes and continents and the ensuing fault reactivations. The impact of climatic changes on sedimentation is also examined.