Ngoc Hien Fm
Type Locality and Naming
Malay Basin. The type section is located borehole Ngoc Hien (GK.46-NH-IX), at depths 1750 to 2526 m (N = 7°08’; E = 104°03>). It was named by Đỗ Bạt 2002
Synonym: Hệ tầng Ngoc Hiền: Đỗ Bạt 2002.
Lithology and Thickness
The stratotype is mainly claystone grading upwards into claystone interbedded with sandstone and some brown coal seams. The thickness of the formation in this borehole is 776 m. In general, the Fm is composed mainly of claystone, in some places, greenish-grey, thickbedded limestone, coaly shale, coal seams with thin interbeds of sandstone and siltstone. Limestone usually contains fossils of forams and other marine faunas. Claystone is rich in organic matter, therefore can be gas source rocks. The members of glauconite-bearing sandstone have been determined as good to very good petroleum reservoir beds with the porosity of about 15-30% and the permeability of over 100 mD.
Relationships and Distribution
Lower contact
Unconformably upon the Kim Long Fm
Upper contact
Conformably under the Dam Doi Fm
Regional extent
It is rather largely distributed in the Malaya - Tho Chu Basin.
GeoJSON
Fossils
Magnastriatites howardi - Echiperiporites estaela Assemblage and the Florschuetzia levipoli Zone of Early Miocene age, Verrucatosporites, Barringtonia, Calamus, FI. trilobata, FI. levipoli, FI. semilobala, Retimonocolpites, Pinus and Rhizophora, some dinoflagellates, and Pediastrum, Acrostichum etc. Nannoplanktons include Discoaster drugii, Heiicosphaera ampliaperta having LAD in NN4 (Early Miocene).
Age
Depositional setting
It is interpreted as a marshy, wet delta plain environment with the abundance of coal seams interbedded with littoral and shallow-sea members.
Additional Information