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朝川组

坐标28°42′N 119°12′E / 28.7°N 119.2°E / 28.7; 119.2
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朝川组
地层年代阿尔布期-森诺曼期
~112–94 Ma
类型
上覆方岩组
下伏早白垩世凝灰岩馆头组磨石山群
厚度高达518米(1,699英尺)
岩性
主要砂岩粉砂岩
次要凝灰岩
地点
经纬度28°42′N 119°12′E / 28.7°N 119.2°E / 28.7; 119.2
地区浙江省
国家 中國
[[file:
朝川组在中國的位置
朝川组
朝川组 (中國)
朝川组在浙江的位置
朝川组
朝川组 (浙江)
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朝川组是位于中国浙江省的一个地层。由紫红色钙质砂屑、泥质粉砂岩、细粒砂岩与凝灰质砂岩、砾岩流纹凝灰岩互层组成。[1]

化石

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从该地层中报告的化石:

参见

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参考资料

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  1. ^ (2009) Chaochuan Formation. In: Zhang S. (eds) Geological Formation Names of China (1866–2000). Springer, Berlin, Heidelberg
  2. ^ Rongjun Chen; Wenjie Zheng; Yoichi Azuma; Masateru Shibata; Tianliang Lou; Qiang Jin; Xingsheng Jin. A New Nodosaurid Ankylosaur from the Chaochuan Formation of Dongyang, Zhejiang Province, China. Acta Geologica Sinica (English Edition). 2013, 87 (3): 658–671 [2023-06-02]. doi:10.1111/1755-6724.12077. (原始内容存档于2022-02-15). 
  3. ^ Z. Dong. 1979. Cretaceous dinosaurs of Hunan, China. Mesozoic and Cenozoic Red Beds of South China: Selected Papers from the "Cretaceous-Tertiary Workshop", Institute of Vertebrate Paleontology and Paleoanthropology & Nanjing Institute of Paleontology (eds.), Science Press, Nanxiong, China 342-350
  4. ^ M.-p. Qian, Z.-y. Zhang, Y. Jiang, Y.-g. Jiang, Y.-j. Zhang, R. Chen, and G.-f. Xing. 2012. [Cretaceous therizinosaurs in Zhejiang of eastern China]. Journal of Geology 36(4):337-348
  5. ^ L. E. Zanno. 2010. Osteology of Falcarius utahensis (Dinosauria: Theropoda): characterizing the anatomy of basal therizinosaurs. Zoological Journal of the Linnean Society 158(1):196-230
  6. ^ Lü Junchang; JIN Xingsheng; SHENG Yiming; LI Yihong; WANG Guoping; Yoichi AZUMA (2007). "New nodosaurid dinosaur from the Late Cretaceous of Lishui, Zhejiang Province, China". Acta Geologica Sinica (English ed.). 81 (3): 344–350. doi:10.1111/j.1755-6724.2007.tb00958.x.