THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN

The marine Oligocene deposits of Pakistan are exposed in the Baluchistan and Lower Indus Basins. The Baluchistan Basin deposits are referred to the Khojak Formation of Makran Group. They represent three planktic foraminiferal zones, the Globigerina ampliapertura Zone, G. ciperoensis Zone and Globoro...

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Main Author: A. A. KURESHY
Format: Article
Language:English
Published: Milano University Press 2020-05-01
Series:Rivista Italiana di Paleontologia e Stratigrafia
Subjects:
Online Access:https://riviste.unimi.it/index.php/RIPS/article/view/13430
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author A. A. KURESHY
author_facet A. A. KURESHY
author_sort A. A. KURESHY
collection DOAJ
description The marine Oligocene deposits of Pakistan are exposed in the Baluchistan and Lower Indus Basins. The Baluchistan Basin deposits are referred to the Khojak Formation of Makran Group. They represent three planktic foraminiferal zones, the Globigerina ampliapertura Zone, G. ciperoensis Zone and Globorotalia kugleri Zone, corresponding to Early, Middle and Late Oligocene. The Lower Indus Basin deposits of Sind include the Kirthar and Nari Formations. On the basis of the larger Foraminifera these deposits are divided into Nummulites fichteli Zone (Early Oligocene), N. fichteli/Lepidocyclina (E.) dilatata Zone (Mid. Oligocene), and L. dilatata Zone (Late Oligocene). The Oligocene deposits are absent in the Upper Indus Basin due to the orogenic movement which took place at the end of the Eocene and continued in the Oligocene.
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spelling doaj.art-825aa89a3a2843b39ebb73b4ebe1cad02023-09-02T17:14:54ZengMilano University PressRivista Italiana di Paleontologia e Stratigrafia0035-68832039-49422020-05-01893THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTANA. A. KURESHYThe marine Oligocene deposits of Pakistan are exposed in the Baluchistan and Lower Indus Basins. The Baluchistan Basin deposits are referred to the Khojak Formation of Makran Group. They represent three planktic foraminiferal zones, the Globigerina ampliapertura Zone, G. ciperoensis Zone and Globorotalia kugleri Zone, corresponding to Early, Middle and Late Oligocene. The Lower Indus Basin deposits of Sind include the Kirthar and Nari Formations. On the basis of the larger Foraminifera these deposits are divided into Nummulites fichteli Zone (Early Oligocene), N. fichteli/Lepidocyclina (E.) dilatata Zone (Mid. Oligocene), and L. dilatata Zone (Late Oligocene). The Oligocene deposits are absent in the Upper Indus Basin due to the orogenic movement which took place at the end of the Eocene and continued in the Oligocene.https://riviste.unimi.it/index.php/RIPS/article/view/13430Biostratigraphy; Foraminifera; Oligocene; Pakistan.
spellingShingle A. A. KURESHY
THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN
Rivista Italiana di Paleontologia e Stratigrafia
Biostratigraphy; Foraminifera; Oligocene; Pakistan.
title THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN
title_full THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN
title_fullStr THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN
title_full_unstemmed THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN
title_short THE OLIGOCENE FORAMINIFERAL BIOSTRATIGRAPHY OF PAKISTAN
title_sort oligocene foraminiferal biostratigraphy of pakistan
topic Biostratigraphy; Foraminifera; Oligocene; Pakistan.
url https://riviste.unimi.it/index.php/RIPS/article/view/13430
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