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Coastal Ocean Studies off Natal, South Africa by E. Schumann, E. Schumann

By E. Schumann, E. Schumann

Mendacity alongside the japanese seaboard of South Africa, the province of Natal has many very important institutions with the sea. there's a significant wealth of knowledge on hand, provided via experts from academia and state-funded examine businesses. hence, this quantity offers the reader with a huge and thorough evaluate of the oceanography of this crucial area of the Southern African beach. This quantity may be of curiosity to a large viewers of oceanographers, marine geologists, and geographers

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26 46 STECKLER , M S an d A B WATTS (1978) . Subsidenc e o f th e Atlantic-typ e continenta l margi n of f Ne w York . Eart h an d Planetar y Scienc e Letters , 41 , 1-13 . TANKARD , A J , M P A JACKSON, K A ERIKSSON, D K HOBDAY , D R HUNTE R an d W E L WINTER (1982) . Crusta l evolutio n o f souther n Africa . Springer-Verlag , Ne w York , 52 3 pp . VAIL, P R , R M MITCHUM R G TODD, J M WIDMIER, S THOMPSON , J B SANGREE , J N BUBB an d W C HATLELID (1977) . Seismi c stratigraph y an d globa l change s o f sea-level .

Paris , 81-111 g shel f sedimen t dispersa l l margin . Marin e Geology , . Th e Cretaceou s an d Tertiar y sedimentar y basin s o f d Zululand . In : Sedimentar y Basin s o f th e Africa n ) G BLANT. Associatio n f Africa n Geologica l Surveys , . FORSTER , R (1975) . Geologica l histor y o f th e sedimentar y basi n o f souther n Mozambiqu e an d som e aspect s o f th e origi n o f th e Mozambique channel . Palaeogeography , palaeocllmatology , an d palaeo-ecology , 17 , 267-287 . FRANKEL , J 0 (1972) .

D a t th e tim e o f rifting s t o th e Earl y Tertiar deca y o f a rift-relate Davies , an d decreas an d i n eas t Africa increas e agai n i n Lat e Tertiary-Recen th e Earl y Cretaceou , O n th e Tugel a Cone , Subsidenc e histor , an d y fro m y i s commensurat e wit h th e bu t renewe d subsidenc Deep-se a sedimentatio e i n sedimentatio Davie s e t al . 1977 ; e i n th e n rate s bot h n rate s i n th e Worsle y an d Variou s reason s fo r thi s hav e bee n given , s o f aluminiu m oxid e sugges t Increase d terrestria Copyright American Geophysical Union.

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