Angren Fm
Type Locality and Naming
Along the Angren River, Prishchekent District, Collective of authors, 1959 (382, table 13). Stratotype by boreholes: 2091, 2097, 2076 in the Angren River valley (367, Appendix 16).
Synonym: Angrenskaya Formation, Ангренская св.
Lithology and Thickness
Interbedding of gravelites, sandstones, clays, and brown coals. Thickness up to 230 m.
Relationships and Distribution
Lower contact
Angren Fm transgressively overlies the Paleozoic, primary weathering crust, or Changan Fm.
Upper contact
With apparent conformity, it is overlain by the Dzhigiristan Fm
Regional extent
GeoJSON
Fossils
Contains large plant remains - Haysmannia leeiana Sze, Marattia müensteri Goepp., Coniopteris ferganensis Pryn., etc., spores, and pollen: from the lower part of the section Coniopteris hymenophylloides (Brongn.), Sew., Marattiopsis muensteri (Goepp.), Phlebopteris polypodioides Brongn., Hausmannia leeiana Sze, Lygodium volubiliopsis Kuz., Protoconiferus funarius (Naum.) Bolch., Bennettites sp., B. modius Bolch., Cecrus aristata Zauer.; from the middle part of the section - Coniopteris hymenophylloides (Brongn.), Sew., Hausmannia leeiana Sze, Osmundopsis angrenica Sixt., Bennettites dilucidus (Bolch.), Ginkgo parva Bolch., Protopinus pergrandis Bolch., Pinus sp.; from the upper part of the section - Coniopteris hymenophylloides (Brongn.), Sew., Phlebopteris polypodioides Brongn., Hausmannia leeiana Sze, Klukisporites variegatus Couper, Plicifera delicata (Bolch.) Bolch., Bennettites ailucidus Bolch., Cycas glabra Bolch., Podocarpus unicus (Bolch.), Classopollis sp. (367, Appendix 16).
Age
Depositional setting
Additional Information