Tamulangou Fm
Type Locality and Naming
It was named by the No. 2 Regional Survey Party under the Geological Bureau of Heilongjiang Province in 1981. The naming section is located at Tamulan Gully southwest of Zuo’er Town, Yakeshi City, Hulunber League, Inner Mongolia. Lowermost formation in Xing'anlin Gr.
Synonym: (塔木兰沟组)
Lithology and Thickness
Tamulangou Fm. is composed largely of grey-green amygdaloidal oligoclase basalt, dense massive oligoclase basalt and their breccias, as well as oligoclase trachyandesite, intercalated with thin layers of grey-black silty mudstone, with a thickness of over 609 m.
Relationships and Distribution
Lower contact
It overlies disconformably the Nanping Fm. However, in Heilongjiang, it is underlain by the Kaikukang Fm (uppermost Emurhe Gr)
Upper contact
It is overlain conformably by the Jixiangfeng Fm
Regional extent
The formation is distributed essentially at the major peak of the Greater Khingan Mts, as well as within the territory of the Hulunber League west of the former and in the area of the Mountain Road Maintenance Squad of the Highway of Heihe City, Heilongjiang Province; in the area of Xifeng Mts; in the area north of the No. 23 Station of a highway maintenance squad and east of the Nenmuo Highway, and in the area north of the No. 21 Station of a highway maintenance squad and of Waluli.
GeoJSON
Fossils
Age
Depositional setting
Additional Information