Edward Sobel (5 results)
- Hardcover
Seller: Wonder Book, Frederick, MD, U.S.A.Wonder Book
Contact seller5-star sellerCondition: Used - Good
£ 25.94
Free ShippingShips within U.S.A.Quantity: 1 available
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
Seller: Chiron Media, Wallingford, United KingdomChiron Media
Contact seller5-star sellerCondition: New
£ 19.37
£ 15.49 shippingShips from United Kingdom to U.S.A.Quantity: Over 20 available
Hardcover. Condition: New.
Published by Milwaukee Art Museum, 1997
- Softcover
Seller: ANARTIST, New York, NY, U.S.A.ANARTIST
Contact seller5-star sellerSoftcover, single sheet folded twice to form 3 panels printed both sides; good condition; moderate rubbing to cover; long crease to edge of all pages.
The Global Circulation of the Atmosphere
Schneider, Tapio (Editor)/ Sobel, Adam H. (Editor)/ Lorenz, Edward N. (Foreward By)
- Softcover
Seller: Revaluation Books, Exeter, United KingdomRevaluation Books
Contact seller5-star sellerCondition: New
£ 87.94
£ 12.50 shippingShips from United Kingdom to U.S.A.Quantity: 2 available
Paperback. Condition: Brand New. 400 pages. 9.75x7.00x0.75 inches. In Stock.
- Hardcover
Seller: Joseph Burridge Books, Dagenham, United KingdomJoseph Burridge Books
Contact seller5-star sellerCondition: New
£ 240.00
£ 27.00 shippingShips from United Kingdom to U.S.A.Quantity: 1 available
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 Ara…bian 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.
