| 词条 | Zapata Formation |
| 释义 |
| name = Zapata Formation | image = | caption = | type = Geological formation | period = Hauterivian | age = Berriasian-Hauterivian | prilithology = Shale | otherlithology = Turbiditic sandstone, pyrite | namedfor = Cerro Zapata | namedby = | region = Magallanes y la Antártica Chilena & Aysén Regions Santa Cruz Province | country = {{CHL}} {{ARG}} | coordinates = {{coord|51.1|S|73.3|W|display=inline,title}} | paleocoordinates = {{coord|51.3|S|36.9|W|display=inline}} | unitof = | subunits = | underlies = Punta Barrosa & Erezcano Formations | overlies = Tobífera & Springhill Formations | thickness = | extent = Magallanes or Austral Basin | area = | map = {{Location map+ | Argentina | relief = 1 | width = 250 | float = center | places = | lat_deg = -51.1 | lon_deg = -73.3 | mark = Green pog.svg | marksize = 12 }} | map_caption = }}Zapata Formation ({{lang-es|Formación Zapata}}) is a sedimentary formation of Lower Cretaceous age in the Magallanes or Austral Basin of Argentina and Chile. Much of the formation is folded and faulted as consequence of the Andean orogeny.[1] In outcrops of the Zapata Formation near Torres del Paine, the southernmost fossil of the ichthyosaur genus Platypterygius has been found.[2][3] References1. ^Fildani et al., 2008 2. ^Pardo Pérez et al., 2012 3. ^Páramo, 2018, p.16 Bibliography
Further reading
15 : Geologic formations of Chile|Geologic formations of Argentina|Lower Cretaceous Series of South America|Cretaceous Argentina|Cretaceous Chile|Fossiliferous stratigraphic units of South America|Paleontology in Chile|Berriasian Stage|Hauterivian Stage|Shale formations|Sandstone formations|Deep marine deposits|Turbidite deposits|Geology of Magallanes y la Antártica Chilena Region|Geology of Santa Cruz Province, Argentina |
| 随便看 |
|
开放百科全书收录14589846条英语、德语、日语等多语种百科知识，基本涵盖了大多数领域的百科知识，是一部内容自由、开放的电子版国际百科全书。