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Abstract

Summary

Oil-proneType I and Type II kerogens, as well as oil/gas prone Type II-III kerogens, considered capable of generating oil and gas at higher maturity within the area.

Biomarker signatures [n-alkanes >n-C25 are dominant, high C29/C30 17α (H) hopane ratios (1.10–3.3) & high C29 steranes (49.0–71.3 %)] and chemical compositions [low total sulfur and V/(V+Ni) ratio] suggest a predominantly terrestrial source input with some contribution from aquatic microorganism as indicated by common occurrence of amorphous organic matter.

© EAGE Publications BV
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/content/papers/10.3997/2214-4609.201801705
2018-06-11
2024-04-25

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References

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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201801705
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Organic Geochemical Characteristics of Tertiary Organic-Rich Sediments from Onshore Penyu Basin, Malaysia
Conference Proceedings 2018, 1 (2018); https://doi.org/10.3997/2214-4609.201801705
/content/papers/10.3997/2214-4609.201801705
/content/papers/10.3997/2214-4609.201801705
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