Ca Coi Fm
Type Locality and Naming
The type section is located at a depth of 1220-2100 m in the CL-1 Borehole, Ca Coi Village, Tra Cu District, Tra Vinh Province (N = 9°33’; E = 106°22’). It was named by
Synonym: Hệ tầng Cà Cỗi: Nguyen Giao 1982; Dỗ Bat 1985, 1993. 2000.
Hệ tầng Cu Lao Dung: Le Van Cu 1982.
Lithology and Thickness
White-grey, violet-reddish, chocolate-colored clastic rocks, such as conglomerate, gritstone, medium- to coarse-grained sandstone containing pebbles and grit, and some claystone. Up to 1 km thick.
Relationships and Distribution
Lower contact
Unconformably rests upon basement of Jurassic andesite, and andesitic tuffs ( Deo Bao Loc Fm ).
Upper contact
Underlies the Tra Cu Fm of early Oligocene.
Regional extent
West Nam Bo, and Cuu Long Basin (offshore).
GeoJSON
Fossils
Pinuspollenites, Pteris, Polypodiaceiosporites, Enica, Gleichenicidites, Podocarpidites, Myricacidites, Triporopollenites, Betuỉaceỉosporítes and Cicatricosisporites, and especially Trũdopoỉỉìs and Plicapollis
Age
Depositional setting
Alluvial and proluvial. It is interpreted as a continental environment (deluvia, proluvia and alluvia) under conditions of high energy of the first stage of subsidence and extension forming the grabens, therefore their distribution area is possibly limited to the slope of some deep troughs of the basin.
Additional Information