
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
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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
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