Published December 9, 2021
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Text-fig. 3. Outcrop cross section of the turbidite facies distribution in the Majalengka, correlated northwest to southeast. The progradation pattern indicated by thickening of sandstone into the basin area are shown. F1 – heterolithic sandstone-mudstone 1; F2 – heterolithic sandstone-mudstone 2; F3 – mudstone facies; F4 – heterolithic fine sand and mudstone; F5 – conglomeratic to massive sandstone facies (Muljana 2012). in Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia
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Text-fig. 3. Outcrop cross section of the turbidite facies distribution in the Majalengka, correlated northwest to southeast. The progradation pattern indicated by thickening of sandstone into the basin area are shown. F1 – heterolithic sandstone-mudstone 1; F2 – heterolithic sandstone-mudstone 2; F3 – mudstone facies; F4 – heterolithic fine sand and mudstone; F5 – conglomeratic to massive sandstone facies (Muljana 2012).
Notes
Published as part of Muljana, Budi, Mardiana, Undang, Hardiyono, Adi, Sulaksana, Nana, Setiadi, Djadjang Jedi & Jurnaliah, Lia, 2021, Lithofacies And Ichnofacies Of Turbidite Deposits, West Java, Indonesia, pp. 1-10 in Fossil Imprint 77 (1) on page 3, DOI: 10.37520/fi.2021.001, http://zenodo.org/record/7167363
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- Journal article: 10.37520/fi.2021.001 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FFC2B24CA8461A48E118CE7AFFB3F506 (LSID)
- Journal article: https://zenodo.org/record/7167363 (URL)