Cau Fm
Type Locality and Naming
Nam Con Son Basin. The type section is located within Hole Dua-IX (Lot 12) from a depth of 3680 to 4038 m (N = 7°36’; E = 109°5’) . It was named as the Cau (areca palm) Fm according to the tradition of naming offshore units.
Synonym: Hệ tầng Cau: Lê Văn Cự 1982, 1985. Điệp Cau: Đỗ Bạt 1986, 1993,2000. Hệ tầng Trà Tán: Ngô Thường San 1981; Võ Dương 1982.
Lithology and Thickness
Mainly grey sandstone interbeddcd with brown claystonc and siltstone. The quartz sandstone is fine- to coarse-grained with poor sorting, carbonate-clayey cement. The total thickncss of the formation in this hole reaches 358 m.
Relationships and Distribution
Lower contact
Unconformably upon rocks of the basement.
Upper contact
Unconformably under the Dua Fm
Regional extent
Nam Con Son Basin.
GeoJSON
Fossils
Florschuetzia trilobata Zone. Characteristic palynomorphs are Florschuetzia trilobata accompanied by Magnastriatites. howardi, Pinuspollenites, Verrucatosporites, Osmunda, Gemmamonoles, Retitricolpites, Cyclophorus, Crudia and forms of the deltaic plain: Barringtonia, Calophyllum, Calamus and freshwater algae Pediastrum, Bosedinia mixed with foraminiferal shells. The Oligocene Florschuetzia trilobata Zone is determined by the presence of FI. trilobata and the absence of other species of Florschuetzia. The Oligocene age has been determined also by Verrutricolpites pachydermus and Mayeripollis
Age
Depositional setting
It was formed in the conditions of fast environmental change in different regions: continental facies in the N-NW and W-SW margins of the basin, deltaic facies and lacustrine-lagoonal in the E part.
Additional Information