anticlinal locally exposure graben biodegradable alkane lacustrine fresh karakter year rich resin material geophysic primarily regionally precursor four palaeogene qiu non condition syn smaller bounded glauconite quantitie quite grey cretaceou when nizar diasterane like batuan habitat data abundant presence molecule pre analyzed dominant complex publication mohave benakat nature producing horizon research prime geoscience lime clarendon origin 2015 email indentified wa coarse type basin different but trap siltstone vol north although event spectrometry geochim PAPER suggest may work licence nebula aim 279 relatively dan west title inferred 1995 conf light addres oxygen will originated calcareou C27 part resource both ACCESS imaging half interbed respectively during sterol paleodepositional consolidated encroached semarang sandy principal collaboration except showing attribution 272 sediment chemical technology any more TRM EP plant cutting top versu oil fault alberdi creating distribution figure citation previou oxidizing nugroho mineral study edu prasetyawati potential cekungan still other white antxon marginal sandstone oligocene industrial basement brown get good induk because relative sumatera dark eocene tight sea universita pattern geophysical doi porosity 1992 sterane siliciclastic akar fine deposition last lower carbonate muslim response biota integrated character aromatic pres diagram thu jamaluddin1 transitional simoneit reflecting carbonaceou biomarker proven marine science online corporation tend downloaded prerequisite analysi understood 110 human trace value trangresion reservoir not supported 22nd mas sumatra blocky maria2 216 model than displaying subroto platy upper indication target view geochemistry OPEN 13C along hole include geokimia rank cemented suseno characterized also input facie used dependent topographic humic determine comparison eubank indonesian geochemical biodegradation colored CRL fuqi1 mining characteristic water however about cros indonesia black prabumulih content 378 erfan must isotope developed selected publishing hard frequently under waple reefal boston readily pristine oxide including opportunitie geology matter combined upc reducing amount china biodegraded stream medium generated just hasanuddin usually large faculty ltd supermassive convention jian break coal sedimentary talang 347 off published normal tectonic common tertiary 2885 junzhi IV high block pleistocene contain originating dipterocarpacceae oxidation specific exploitation south structure coster increase correlation boundarie source stratigraphy melalui dengan minyak special depositional chengfuqi fang 745 fluviatile cite predominated implication update control deposit barisan cosmochim jie star miocene sedimentation IOP 2688 term should enhancement main massive conference maintain it consist annual air environmental use C17 hydrocarbon beneath late streak taken lemat southeast school care mountain form regressive open 21st akiyama conclude surface stratigraphic emi land level affect while lampung such indicate abstract sunda asia bitumen overlying two enim SMT associated estimate paralic characterization C28 continued well parameter subdivision gmail mature saturated yong silty uplifted oxic fowler became composition grain mujahindin one resultant understanding baturaja ga hutchison occur unpublished styrene compression acta potentially international C18 organic diponegoro introduction triterpene triangular zakaria armstrong bottom IPA aulia qingdao between 739 earth association conclusion department angular gobi 27168B environment very beiruny coast rounded journal jamaluddin terrestrial ser ecological according syamsuddin2 transgressive 2011 1956 sample plain proposed shallow kerogen together using change MS asymmetric classification oxidative evaluate similarly done platform hundred changing location namely case ratio jambi 1979 generally reflected relationship composed krisna setyawan structural first regression existing analyze shale protoplanetary com maturation sio ha 222 palembang significant muara contribution area GC mathematic oxford makassar dominance fan plio algae porou dominated proceeding east sci shelf derived toward geological 325 1993 method studied compound megacycle pulunggono deltaic clear highly slight compared studie heidrick carried 3rd addition DOI 14th lapangan characterize depression carbon proces william most analyse 114 chromatography began time 27168 fraction survey limestone result serie namib indicator 1315 clay lambiase coaly triterpane central low δ13C min giving kasim kalahari mixed antara show huang brassell acyclic boundary further 1088 into palaeoenvironmental represented sundaland diagenetic early maturity based environ society lahat having sub identify down especially discussion obtained contribute alluvial reference IP photosynthetic number shanghuo isoprenoid meinschein group play formation filling exploration sorted umar3 1978 plot active better M87 layer earth' starting korelasi cheng 1974 divided region 2019 spruyt rift provide wang constituted stone reflect therefore sequence found abudance correlated minor speek selatan system jamaljamaluddin1994 1985 petroleum 282 telisa considered wax braided idea containing article didyk asian some produce 337 three zhang middle all now rock teguh crude give depth nomenclature bumi out contained deposited coastal 1996 bacteria ranging gradually kazunori brackish map telescope connection 241 thermal field until engineering pristane higher 1755 2023 produced delta 156 C29 university development phytane biological kasai range aquatic 012024 interpretation related within fluvio author creative prospect specie eglinton