Huadian Fm
Type Locality and Naming
The naming section is located at Gonglangtou and Daboji ~15 km northeast of Huadian County, Jilin. Named by Nishita Shouichi in 1940.
Lithology and Thickness
This formation may be divided into three parts: Lower part, yellowish brown or gray sandstone and pebbly sandstone with carbonaceous shale; Middle part, yellowish brown sandstone with variegated sandstone and mudstone, with several beds of minable oil shale; Upper part, grayish white, grayish green and gray pebbly sandstone, sandstone, muddy sandstone and sandy mudstone, with oil shale and lignite beds. The outcrops are generally poor, mainly found in the wells; the thickness reaches 1600–1900 m.
Relationships and Distribution
Lower contact
Unconformable contact with both the underlying Early Cretaceous Heiweizi Fm or Paleozoic granite and metamorphic series.
Upper contact
Unconformable contact with the overlying Tumenzi Fm.
Regional extent
This formation is mainly distributed at Gonglangtou, Zaiboji, Miaoling, Beitaizi, Xitaizi and Zhongxinjie, Huadian County.
GeoJSON
Fossils
Fossils of the Huadian Formation are only found in its middle and upper parts. In addition to plants, gastropods and Threskiorothidae and Anatidae of birds, the fishes are mainly Amia, Catostomidae and Clupeiformes, and the mammals mainly include Eochenus sinensis, Tupaiodon huadianensis, Ernosonex jilinensis, Asiomomys changbaicus and Zelomys orientalis.
Age
Depositional setting
According to the fauna, flora and sediments, the ecological environment of Huadian then was of forest-swamp-lake facies. A number of animals living in tropical and subtropical jungles appeared; meanwhile, there were numerous fishes and hydrophilic birds.
Additional Information