论文信息 - The diagenesis of continental (Karoo—Tertiary?) siliciclastics from an East African rift valley (Rukwa—Tukuyu area), Tanzania—discussion - 字舞流文

The diagenesis of continental (Karoo—Tertiary?) siliciclastics from an East African rift valley (Rukwa—Tukuyu area), Tanzania—discussion

[1] H. Dypvik,et al. The diagenesis of continental (Karoo-Tertiary?) siliciclastics from an East African rift valley (Rukwa-Tukuyu area), Tanzania , 1992 .

[2] C. Morley,et al. Geology and geophysics of the Rukwa Rift, East Africa , 1992 .

[3] S. Cunningham,et al. New Biostratigraphic Age Dates from the Lake Rukwa Rift Basin in Western Tanzania: Geologic Note (1) , 1991 .

[4] C. Ebinger. Tectonic development of the western branch of the East African rift system , 1989 .

[5] John W. Peirce,et al. Structural interpretation of the Rukwa Rift, Tanzania , 1988 .

[6] J. Chorowicz,et al. East African rift system: offset, age and tectonic significance of the Tanganyika-Rukwa-Malawi intracontinental transcurrent fault zone , 1988 .

[7] F. Dixey. The Nyasaland Section of the Great Rift Valley , 1926 .

[8] P. Aagaard,et al. Upper paleozoic and Pesozoic sedimentation in the Rukwa-Tukuyu Region, Tanzania , 1990 .

[9] E. Fourtanier. Diatomees neogenes d'afrique : approche biostratigraphique en milieux marin (sud-ouest africain) et continental , 1987 .