Fangyan shakllanishi - Fangyan Formation - Wikipedia
| Fangyan shakllanishi Stratigrafik diapazon: Kechki bo'r, 100.5–85 Ma | |
|---|---|
| Turi | Shakllanish |
| Aslida | Chaochuan shakllanishi va Moshishau guruhi |
| Haddan tashqari | Guantou shakllanishi va Zhaochuan shakllanishi |
| Qalinligi | 1700 metrgacha (5600 fut) |
| Litologiya | |
| Birlamchi | Konglomerat |
| Manzil | |
| Mamlakat |  Xitoy |
The Fangyan shakllanishi a geologik shakllanish yilda Xitoy (Dongyang ). Bu asosan iborat konglomeratlar. U saqlaydi dinozavr davridan qolgan toshqotganliklar Kechki bo'r.[1]
Paleofauna
Holotip Dongyangosaurus, Fangyan shakllanishidan
Adabiyotlar
- ^ Qilingan Pol; Barret, Pol M.; Dodson, Piter (2004). Vayshampel, Devid B.; Dodson, Piter; Osmolska, Xalska (tahr.) Dinozavrlar (2-nashr). Berkli: Kaliforniya universiteti matbuoti. ISBN 978-0-520-24209-8.
- ^ Lu Junchang; Yoichi Azuma; Chen Rongjun; Chjen Venji; Jin Xingsheng (2008). "Chjetszyan viloyati, Dongyangning so'nggi bo'r davridan yangi titanosauriform sauropod". Acta Geologica Sinica (ingliz nashri). 82 (2): 225–235. doi:10.1111 / j.1755-6724.2008.tb00572.x.
- ^ Qilingan Pol; Barret, Pol M.; Dodson, Piter (2004). "Sauropoda ". Vayshampelda Devid B.; Dodson, Piter; Osmolska, Xalszka (tahr.). Dinozavrlar (2-nashr). Berkli: Kaliforniya universiteti matbuoti. ISBN 978-0-520-24209-8.