Lake Type & Lacustrine Facies Association	Stratigraphy	Source Potential	Hydrocarbon Characteristics
OVERFILLED Fluvial-Lacustrine Facies Association	Maximum progradation: Parasequences related to lateral progradation (relatively subtle) Maximum fluvial input	Low to moderate TOC Mixed Type I-III kerogen Marked organic facies contrasts Distinct lateral changes in organic facies	Generate both oil and gas Very waxy, low-sulfur oils Terrigenous biomarker assemblage dominant
BALANCED-FILL Fluctuating-Profundal Facies Association	Mixed progradation and desiccation: Distinct shoaling cycles common Fluvial input variable	Moderate to high TOC Predominantly Type I kerogen, with Type I-III mixtures near flooding surfaces Relatively homogenous and laterally consistent organic facies	Mostly oil generative Paraffinic but relatively non-waxy oils; low sulfur Algal biomarker assemblage dominant
UNDERFILLED Evaporative Facies Association	Maximum desiccation: High-frequency wet-dry cycles Minimum fluvial input	Low overall TOC (w/ some high TOC intervals) Type I kerogen Minimum organic facies contrasts Laterally consistent organic facies	Mostly oil generative Paraffinic oils; moderate to high sulfur Distinctive "hypersaline" biomarker assemblage