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Maonong Formation

Maonong Fm


Period: 
Jurassic

Age Interval: 
Middle Jurassic, (TJ89)


Province: 
Zhejiang

Type Locality and Naming

It was named by Wu Zhizhun, Zhan Xikun, Zhu Fuwu as the “Maonong Coal-bearing Member” in 1961. The naming section is located at the Maonong Coal Mine, Jingjukou area, Songyang County, Zhejiang Province.

Synonym: (毛弄组)


Lithology and Thickness

Lower member represents dacitic pebble-bearing crystal vitric tuffs, intercalated with a small amount of thin-bedded pebble-bearing sandstones, with its lower part containing occasionally lenticular coal beds, with a thickness of over 400 m. Upper member represents an alternating layer of sandy conglomerates in association with sandstones, siltstones, shales and carbonaceous shales, intercalated with coal beds, with a thickness of about 460 m.


Lithology Pattern: 
Volcanic ash


Relationships and Distribution

Lower contact

The relationship between its basal part and the underlying Longpu Fm is unknown (with no base having been found).

Upper contact

Regionally, the schematic strat column indicates the next younger unit is a volcanic-sedimentary unit of Baiyancun Fm of late Jurassic. However, it may be disconformably overlain by the early Cretaceous Moshishan Gr (Dashuang Fm).

Regional extent

The formation is distributed largely in the Maonong and Xiaocha areas of Songyang County, the Yangjia Mt of Yunhe County, and the Zhucun and Yangcun Villages of Lishui County.


GeoJSON

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Fossils

It yields bivalve fossils such as Ferganoconcha aff. estheriaeformis and F. cf. subcentralis; and plant fossils as represented by a middle-stage assemblage of the Coniopteris-Phoenicopsis flora, whose important members are Neocalamites carrerei, Coniopteris hymenophylloides, Eboracia lobifolia, Baiera furcata and Phoenicopsis spp.


Age 

Schematic strat column in previous "red Chinese Lexicon" had implied that the Maonong Fm spanned the Middle Jurassic. Chen et al. (2007) and Liu L et al. (2012) reported SHRIMPand LA-ICP-MS zircon U-Pb dates to be 180 and 177 Ma, respectively, on dacite tuff horizons in this formation (Guangfu Xing, Jianqing Li, Zheng Duan, Mingxuan Cao, Minggang Yu, Pingli Chu, Rong Chen. Mesozoic–Cenozoic Volcanic Cycle and Volcanic Reservoirs in East China. Journal of Earth Science, 2021, 32(4): 742-765. doi: 10.1007/s12583-021-1476-1). This would suggest it begins at least by mid-Toarcian and perhaps terminated in the Callovian (used here)

Age Span: 

    Beginning stage: 
Toarcian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
179.45

    Ending stage: 
Callovian

    Fraction up in the ending stage: 
1.0

    Ending date (Ma):  
161.53

Depositional setting

The formation belongs to deposits of volcanic-eruption facies and intermontane lacustrine-swamp facies.


Depositional pattern:  


Additional Information


Compiler:  

Jingeng Sha (coordinator)