2020
DOI: 10.18520/cs/v119/i5/831-840
|View full text |Cite
|
Sign up to set email alerts
|

Ooid Fabric in the Jurassic of the Indus Basin, Pakistan: Control on the Original Mineralogy

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2021
2021
2022
2022

Publication Types

Select...
3

Relationship

1
2

Authors

Journals

citations
Cited by 3 publications
(2 citation statements)
references
References 0 publications
0
2
0
Order By: Relevance
“…The Datta Formation is documented to have been deposited in continental settings, forming an unconformable contact, either with the underlying Triassic Kingriali Formation or Pre‐Cambrian rocks and is conformably overlain by the Shinawari and Samana Suk formations (Hashmi, Jan, Khan, & Ali, 2018). The Lower Jurassic Shinawari Formation has an interbedded sequence of shales, marls, sandstones, and limestones, representing shallow to deep marine environments (Ali et al, 2020). The overlying Samana Suk Formation is mainly represented by shallow marine carbonates with some sandstone, siltstone, and mudstones, and has preserved a diverse fauna such as bryozoans, molluscs, brachiopods, ostracods, pollen, and spores.…”
Section: Geology Of the Areamentioning
confidence: 99%
See 1 more Smart Citation
“…The Datta Formation is documented to have been deposited in continental settings, forming an unconformable contact, either with the underlying Triassic Kingriali Formation or Pre‐Cambrian rocks and is conformably overlain by the Shinawari and Samana Suk formations (Hashmi, Jan, Khan, & Ali, 2018). The Lower Jurassic Shinawari Formation has an interbedded sequence of shales, marls, sandstones, and limestones, representing shallow to deep marine environments (Ali et al, 2020). The overlying Samana Suk Formation is mainly represented by shallow marine carbonates with some sandstone, siltstone, and mudstones, and has preserved a diverse fauna such as bryozoans, molluscs, brachiopods, ostracods, pollen, and spores.…”
Section: Geology Of the Areamentioning
confidence: 99%
“…The deposition has resulted in development of a thick sequence of middle Mesozoic rocks (10 to >2,000 m) dominated by calcareous content and depicts variation in lithologies in the inter‐ and intra‐basinal stratigraphic set up. Researchers (e.g., Ahmad et al, 2019; Ali et al, 2020; Ali, Haneef, Anjum, Hanif, & Khan, 2013; Hussain et al, 2013; Nizami & Sheikh, 2009; Qureshi, Butt, & Ghazi, 2008; Saboor, Haneef, Hanif, & Swati, 2020; Shah, Rahim, Hassan, Mustafa, & Ahmad, 2020; Wadood et al, 2020) have portrayed the microfacies and depositional environments of the Middle Jurassic carbonate unit in various sections of the Upper and Lower Indus basins. In terms of palaeoenvironments, they have been interpreted as ranging from tidal flat‐lagoon complex to shoals, beaches, and middle to outer ramp environments.…”
Section: Introductionmentioning
confidence: 99%