Next Article in Journal / Special Issue
Provenance of Late Paleozoic-Mesozoic Sandstones, Taimyr Peninsula, the Arctic
Previous Article in Journal
Nd Isotope Mapping of Crustal Terranes in the Parent-Clova Area, Quebec: Implications for the Evolution of the Laurentian Margin in the Central Grenville Province
Previous Article in Special Issue
Volcanosedimentary Basins in the Arabian-Nubian Shield: Markers of Repeated Exhumation and Denudation in a Neoproterozoic Accretionary Orogen
Geosciences 2013, 3(3), 466-501; doi:10.3390/geosciences3030466
Article

Lower Paleogene Tectonostratigraphy of Balochistan: Evidence for Time-Transgressive Late Paleocene-Early Eocene Uplift

1
 and 2,*
Received: 1 June 2013; in revised form: 19 July 2013 / Accepted: 19 July 2013 / Published: 29 July 2013
(This article belongs to the Special Issue Sedimentary Basins and Orogenic Belts)
View Full-Text   |   Download PDF [4004 KB, uploaded 29 July 2013]   |   Browse Figures
Abstract: Analysis of lithofacies, paleoflow directions, and sandstone petrography of upper Paleocene-lower Eocene paralic and continental sediments exposed along the transpressional suture zone of the western margin of the Indian plate indicate that the process of deformation and uplift of the carbonate shelf in this area had started by late Paleocene time. This tectonic uplift and deformation is documented by: (1) an overall shallowing upward synorogenic sequence of sediments, (2) proximal conglomerate facies (consisting of lower Paleocene and Mesozoic clasts) dominating in the western part of the study area and distal facies of sandstone and shale dominating in the eastern part of the study area, (3) the existence of an unconformity of late Paleocene-early Eocene age in the Quetta and Kalat regions, (4) paleocurrent directions in deltaic and fluvial deposits indicating southeastward flowing sediment dispersal paths during late Paleocene-early Eocene time, which is opposite to that found in the late Cretaceous, suggesting a reversal in the depositional slope of the Cretaceous shelf, and (5) petrographic study of sandstones indicating a collision suture/fold thrust belt provenance. This episode of uplift and deformation could be the result of India-Arabian transpression with associated ophiolite obduction or, more likely, to represent the local response to initial India-Asia contact. The unroofing pattern and uplift geometry of the western Indian shelf suggests that this tectonism first started in the southern part of the study area (Kalat-Khuzdar area) during the late Paleocene-early Eocene and proceeded northward in a time-transgressive fashion.
Keywords: India; Asia; Pakistan; tectonics; stratigraphy; Paleogene; India-Asia collision; Paleocene; Eocene India; Asia; Pakistan; tectonics; stratigraphy; Paleogene; India-Asia collision; Paleocene; Eocene
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Export to BibTeX |
EndNote


MDPI and ACS Style

Khan, I.H.; Clyde, W.C. Lower Paleogene Tectonostratigraphy of Balochistan: Evidence for Time-Transgressive Late Paleocene-Early Eocene Uplift. Geosciences 2013, 3, 466-501.

AMA Style

Khan IH, Clyde WC. Lower Paleogene Tectonostratigraphy of Balochistan: Evidence for Time-Transgressive Late Paleocene-Early Eocene Uplift. Geosciences. 2013; 3(3):466-501.

Chicago/Turabian Style

Khan, Intizar H.; Clyde, William C. 2013. "Lower Paleogene Tectonostratigraphy of Balochistan: Evidence for Time-Transgressive Late Paleocene-Early Eocene Uplift." Geosciences 3, no. 3: 466-501.


Geosciences EISSN 2076-3263 Published by MDPI AG, Basel, Switzerland RSS E-Mail Table of Contents Alert