By T. S. Ahlbrandt, Michael E. Brookfield
ISBN-10: 0444422331
ISBN-13: 9780444422330
Papers disguise the whole spectrum of eolian investigations, starting from the microscopic point to local synthesis in addition to historical eolian deposits and their interpretation
Read Online or Download Eolian Sediments and Processes PDF
Best petroleum books
Pressure Build Up and Flow Tests in Wells - download pdf or read online
E-book by means of C. S. Matthews, D. G. Russell
Elements of petroleum geology - download pdf or read online
This moment variation of components of Petroleum Geology is totally up-to-date and revised to mirror the large alterations within the box within the fifteen years because book of the 1st variation. This e-book is a usefulprimer for geophysicists, geologists, and petroleum engineers within the oil who desire to extend their wisdom past their really expert sector.
Extra info for Eolian Sediments and Processes
Example text
Geog. , 9: 278309. H e d i n , Sven, 1896. A j o u r n e y t h r o u g h t h e Takla-Makan D e s e r t Chinese Turkistan. Geog. , 8: 264-278. 1968. , Sea. G e o l o g i e e n Mijnbouw, 47: 245-273. 1981. A. SOC. Econ. P a l e o n t o l o g i s t s and M i n e r a l o g i s t s Spec. Pub. 31: pp. 315-329. , 1962. L a r g e s u b m a r i n e sand waves. S c i e n c e , 136: 839-848. , 1981. S i g n i f i c a n c e o f i n t e r d u n e d e p o s i t s and bounding s u r f a c e s i n e o l i a n dune sands.
Primary p o r o s i t y of t h e g r a i n f a l l s t r a t a was v a r i a b l e b u t g e n e r a l l y was i n t e r m e d i a t e between t h e r i p p l e and a v a l a n c h e p o r o s i t i e s , with an a v e r a q e of 4 3%. Avalanche s t r a t i f i c a t i o n Avalanche s t r a t i f i c a t i o n i s produced by t h e r e d e p o s i t i o n w a i n f a l l d e p o s i t s by slumpinq or sandflow. q e n e r a l l y heqan a s a slump h l o c k , which sandflows a s i t proceeded downslope.
1971). T h r u s t - t y p e s t r u c t u r e s formed d u r i n q a n a v a l a n c h e can be observed i n p e e l s hetween the structurps deposits. boundinq are formed surfaces as a of slump a n avalanche s t r a t u m ( F i q . 6 ) . block overrides pre-existing These avalanche 47 F i r r . 6. T h r u s t s t r u c t u r e s f o r m e d d u r i n q s l r r m p i n q on t h e s i m u l a t e d f o r e s e t slope. Thpse s t r u c t u r e s a r e commonly f o r m e d a b o u t m i d - s l o p e above t h e a r e a where slumps d e q e n e r a t e t o s a n d f l o w s .
Eolian Sediments and Processes by T. S. Ahlbrandt, Michael E. Brookfield
by David
4.0