Coal petrology of Neogene low-rank coal in Mukah Coalfield, Sarawak, Malaysia: Implications for coal facies and paleodepositional reconstructions
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
https://link.springer.com/content/pdf/10.1007/s12517-022-09519-z.pdf
Reference70 articles.
1. Abdullah Wan Hasiah (1997a) Common Iiptinitic constituents of Tertiary coals from the Bintulu and Merit-Pila coalfield, Sarawak and their relation to oil generation from coal. Bulletin of the Geological Society of Malaysia 41:85–94. https://doi.org/10.7186/bgsm41199708
2. Abdullah WH (1997b) Evidence of early generation of liquid hydrocarbon from suberinite as visible under the microscope. Org Geochem 27 (7-8): 591–596. https://doi.org/10.1016/S0146-6380(97)00085-5
3. Abdullah WH (2002). Organic petrological characteristics of limnic and paralic coals of Sarawak. Bull Geo Soc Malays 45: 65–69.
4. Amijaya H, Littke R (2005) Microfacies and depositional environment of Tertiary Tanjung Enim low rank coal, South Sumatra Basin, Indonesia. Int J Coal Geol 61:197–221. https://doi.org/10.1016/j.coal.2004.07.004
5. Anderson JAR (1964) The structure and development of the peat swamps of Sarawak and Brunei. J Trop Geo 18:7–16
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1. Assessing the Depositional Environment of Cretaceous Ge-Rich Coals in the Wulantuga Mine, Shengli Coalfield, Northeastern China;Energy & Fuels;2024-01-25
2. Petrology of the A and B Seams, Ermelo Coalfield (South Africa): Indications for changing palaeoenvironmental and sedimentary conditions;International Journal of Coal Geology;2022-11
3. Paleoenvironment reconstruction and peat-forming conditions of Neogene paralic coal sequences from Mukah, Sarawak, Malaysia;Scientific Reports;2022-05-25
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