File:Chilcatay and Pisco formations outcrops.jpg

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English: Annotated panoramic photographs of Pisco outcrops showing: (a) eastward view of the upper part of the Chilcatay Formation overlain along an unconformably contact by the marine deposits of the P0 allomember at Cerro los Tinajones (circled geologist for scale); (b) the vertically staked marine deposits of P0 and P1 at Cerro Submarino (circled car for scale); (c) outcrop view ofsediments in the vicinity of the unconformity surface between allomembers P1 and P2 (PE0.2) at Cadenas de los Zanjones; (d) crystalline basement nonconformably overlain by P1 strata and ledge-forming marker beds within P1 and P2 (Cerro la Bruja); (e) crystal-line basement nonconformably overlain by P2 strata and ledge-forming marker beds serving as formidable correlation tools overwide areas within P2 (Cerro Hueco la Zorra).
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Source Di Celma, Claudio, et al. (2018). Intraformational unconformities as a record of late Miocene eustatic falls of sea level in the Pisco Formation (southern Peru). Journal of Maps. 14. 607-619. https://www.tandfonline.com/doi/full/10.1080/17445647.2018.1517701
Author Claudio Di Celma, Elisa Malinverno, Giulia Bosio, Karen Gariboldi, Alberto Collareta, Anna Gioncada, Walter Landini, Pietro Paolo Pierantoni & Giovanni Bianucci

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current15:08, 7 April 2023Thumbnail for version as of 15:08, 7 April 20231,500 × 1,867 (823 KB)PaleoNeolitic (talk | contribs)Uploaded a work by Claudio Di Celma, Elisa Malinverno, Giulia Bosio, Karen Gariboldi, Alberto Collareta, Anna Gioncada, Walter Landini, Pietro Paolo Pierantoni & Giovanni Bianucci from Di Celma, Claudio, et al. (2018). Intraformational unconformities as a record of late Miocene eustatic falls of sea level in the Pisco Formation (southern Peru). Journal of Maps. 14. 607-619. https://www.tandfonline.com/doi/full/10.1080/17445647.2018.1517701 with UploadWizard

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