Seca Formation, Ekvador - Seca Formation, Ecuador
| Seca shakllanishi Stratigrafik diapazon: Kech Eosen (Divisaderan -Tinguirirican ) ~37–34 Ma | |
|---|---|
| Turi | Geologik shakllanish |
| Birligi | Ancón guruhi |
| Aslida | Punta-Ankon shakllanishi |
| Haddan tashqari | Socorro shakllanishi |
| Litologiya | |
| Birlamchi | Slanets |
| Manzil | |
| Koordinatalar | 2 ° 18′S 80 ° 48′W / 2,3 ° S 80,8 ° VtKoordinatalar: 2 ° 18′S 80 ° 48′W / 2,3 ° S 80,8 ° Vt |
| Taxminan paleokoordinatlar | 4 ° 48′S 73 ° 48′W / 4.8 ° S 73.8 ° Vt |
| Mintaqa | Santa Elena viloyati |
| Mamlakat |  Ekvador |
| Hajmi | Progreso havzasi |
  Seca Formation, Ekvador (Ekvador) | |
The Seca shakllanishi a Kech Eosen (Divisaderan ga Tinguirirican ichida SALMA tasnifi ) geologik shakllanish ning Progreso havzasi janubi-g'arbiy qismida Ekvador. The slanets hosil bo'lgan dengiz iloni Pterosfen sheppardi.[1]
Tavsif
Seca Formation, qismi Ancón guruhi, mos ravishda ustiga Socorro shakllanishi va bilan qoplangan Punta-Ankon shakllanishi. Seca Formation kulrangdan yashil ranggacha slanets dengiz osti muxlislari bilan dengiz platformasida saqlangan atrof-muhit.[2] Shakllanish a suv ombori jinsi,[3] va potentsial manba jinsi,[4] neftga boy Progreso havzasida.
Shuningdek qarang
Adabiyotlar
Bibliografiya
- Lorenzo, Erika va boshq. 2018. Correlación geoquímica entre crudos y rocas del sistema petrolero de la península de Santa Elena y el golfo de Guayaquil. Boletin de Geologiya 40. 31-42. Kirish 2018-09-11.
Qo'shimcha o'qish
- R. Xoffstetter. 1958. Un serpent marin du janr Pterosfen (Pt. Sheppardi nov. Sp.) Dans L'Éocène supérieur de L'Équateur (Amérique de Sud). Byulletin de la Société Géologique de France 6: 45-50