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Supplemental Material: Geological architecture and history of the Antigua volcano and carbonate platform: Was there an Oligo–Miocene lull in Lesser Antilles arc magmatism?

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posted on 04.08.2022, 17:39 authored by Lei Liu, Hongxiang Guan, Nengyou Wu, et al.

Figure S1: Partial gas chromatograms (FID) of hydrocarbon fractions of samples D2-1(A) and T15-1(B) from the Okinawa Trough. Figure S2: Partial gas chromatograms (FID) of alcohol fractions from samples D2-1(A) and T15-1(B) from the Okinawa Trough. Figure S3: Partial gas chromatograms (FID) of carboxylic acid fractions of samples D2-1(A) and T15-1(B) from the Okinawa Trough. Table S1: Contents and stable carbon isotopic composition of hydrocarbons from the Okinawa Trough seep carbonates. Table S2: Contents and stable carbon isotopic composition of alcohols from the Okinawa Trough seep carbonates. Table S3: Contents and stable carbon isotopic composition of fatty acids from the Okinawa Trough seep carbonates. Table S4: The contents of selected major elements, trace elements and enrichment factors of the Okinawa Trough seep carbonates in this study.

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