Facies and bed type characteristics of channel‐lobe transition deposits from the Oligocene‐Miocene Tajau Sandstone Member, Kudat Formation, Sabah, Malaysia-Reference-Cited by-同舟云学术

Facies and bed type characteristics of channel‐lobe transition deposits from the Oligocene‐Miocene Tajau Sandstone Member, Kudat Formation, Sabah, Malaysia

Published:2021-09-21 Issue:11 Volume:56 Page:5642-5672
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Mansor Hafzan Eva¹²^ORCID,Amir Hassan Meor Hakif¹

Affiliation:

1. Department of Geology, Faculty of Science University of Malaya Kuala Lumpur Malaysia

2. Department of Geoscience, Faculty of Earth Science University Malaysia Kelantan Jeli Malaysia

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4263

Reference212 articles.

1. Tectonostratigraphic terranes of Kudat Peninsula, Sabah

2. Tectonostratigraphic terranes of Kudat Peninsula, Sabah

3. Bedforms and associated sedimentary structures formed under supercritical water flows over aggrading sand beds

4. Anatomy of turbidites and linked debrites based on long distance (120 x 30 km) bed correlation, Marnoso Arenacea Formation, Northern Apennines, Italy

5. Deep-Marine Pseudo Dune Cross-Stratification—Similar, But Completely Different

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