Laserfiche WebLink
IiLli :'I <br />III IIIIIIIII IIII III .~ <br />999 - <br />Combined microbial, seismic ~, N~~e; <br />C~~'e~to~'s <br />surveys predict oil and gas ~ X~ : ~ ~ ~~ <br />occurrences in Bolivia ~~~;E-'~--~5 <br />Jorge Pareja Lopez 1'ncirrtirnfos Petroliferos Fi;cnlrs Bolir'ianos Smrtn Cru_, 6olie'ia <br />Daniel Hitzman, James Tucker Gen-A~icrobinl Trrlrnologirs Inc. Ochrlntn, Okln. <br />icrohial and geophrsinil sur- <br />yers in the jmrgles of Boliv- <br />ia's estencice Sub-Andean <br />region bare combined for <br />three ttlccessful predictions of deep <br />i,il and gas resen~es in as many tries. <br />Hcdrocarbon microseepage mea- <br />surdd by microbial soil samples pre- <br />dicted the Carrasco, Katari, and Sur- <br />ubi structures of Bolivia's Chapatti re- <br />gion in 1991-9?, detecting traps with <br />reserves at depths exceeding -1,500 m. <br />Approximately S00 km of seismic <br />lines covering 3,300 sq km was com- <br />pleted by 1'acimientos Petroliferos Fis- <br />cales Boliyianos (YPFB) for evaluation <br />of the YPFB resen~e block adjacent to <br />\1a~us Energy's 1`lamore block in the <br />Foothills Belt area behreen Santa Cruz <br />and Cochabamba (Fig. 1). <br />For 1 month each rear at the end of <br />the field season, seismic lines were <br />quickly traversed h}' several microbial <br />sampling teams. Using hand augers or <br />shovels, the teams collected more <br />than 3,?00 samples approximately 20 <br />cm (S in.) deep at intervals of 250 m <br />nest to staked seismic locations. <br />Microbial results mere directly com- <br />pared r+'ith seismic profiles for identi- <br />fication and ranking of tra}'s and <br />structures. For the second rear of the <br />seismio-microbial study, the locations <br />of fill-in and extension seismic lines <br />were partially based on the previous <br />year's microbial results. <br />Prospect predictions <br />Two YPFB seismic structures dear <br />onstrated elevated microseepage and <br />were predicted to be productive prior <br />to drilling.' <br />The Carm<co wildcat, drilled to a <br />total depth of -1,770 m, initially pro- <br />duced S57 b/d of condemate and 625 <br />\lcfd of gas from the Tertio rv of l,'_ci~ <br />m and the Devonian at a,i;i m (Fig. <br />?). <br />The Katari ryildcat ryas drilled to a <br />total depth of ~I,94] m and produced <br />607 h'd of oil and 391 \Icfd of gas from <br />Fiy. 1 <br />la Paz ,~`..;;•: <br />~.. . <br />. ~ Cochabamba ~~ <br />BOIIV <br />r <br />i <br />I, I I I I I YPFB Ivirza ,~ Maxus <br />Prospect ~ <br />) ~ j~ Surubi <br />i ~tlt ,' ~t ~ \V1„" ~ Al V ' <br />I i <br />t II r' <br />~ ` 11 ~ 1"~ t ~. ) <br />u `` YPFB Carrasco ~ r; j <br />" 1 \\111 \Katari ~. ' <br />I <br />1 ~... .... ~ ~ ....... <br />:- jis® <br />1: <br />the Deaonian at -1,x-33 m (Fig. 2). <br />A 1 day microbial sun~ev traversing <br />2? km of a Afaaus seismic line crossed <br />the Surubi structure and rcell location <br />prior to drilling. <br />t1'ith microbial anomalies similar to <br />the YPFB study area, the Surubi loca- <br />uon was predicted to be successful <br />(Fig. ~). <br />The Surubi Xo. 1 teas tested from <br />hco zones at o combined rate of S00 <br />b/d of condensate and 9 \Icfd of gas. <br />Additional deviations from the Surubi <br />location hate been completed. <br />Microhiaf approach <br />The Microbial Oil Bootie Technique <br />(~.\105T) used in these ~u n~eys u~as <br />dccaloped L'}' Phillips Pr!mleum Co. <br />in the 1950s to be Oe~ible in the field, <br />uncomplicated in the lab, and accurate <br />^< an nrl and y.t< prcdic;ion tool. <br />In order to indico tr the presence of <br />h;;ht hvdrocorbtms (C;-C;) rMOST <br />nmasu rcs si Ana hoc micn~bial popula- <br />tions, tchich idantily anomalous he- <br />drucarbon micri~srepagc from onshore <br />and offshore oil and gas reser- <br />voirs.'-"s <br />Anomalous h}'drocarbon micro- <br />seeps are identified by observing <br />t`tOST population concentrations and <br />distribution patterns within a survey <br />area.° Anomalous thresholds mere nr <br />terpreted for Bolivia's Sub-Andean re- <br />gion. \h'ell predictions were based on <br />the location and intensity of these <br />threshold anomalies. <br />Prior to final seismic interpretation, <br />microbial data indicated a large and <br />intense microseepage pattern in the <br />western portion n( the YPFB resen•e <br />block along the Ivirza structure. Sub- <br />sequent compm'isun behveen microbi- <br />al anomalies and the geophysical data <br />shmrs o very large target, which has <br />been earmarked for future drilling by <br />1'f FB (Fig. ~). •~ <br />Used in conjunction with sec<••~~' <br />c,vnpaigns and data, the micrnh::l <br />surveys proved to be effective predic- <br />lice tools for identifying productive <br />structures, The lots impact field strate- <br />:;y n( microbial srlrveys proved to be <br />very <br />rain. <br />Ackn <br />Tht <br />de E <br />Geu-1 <br />relea• <br />i OGJ` <br />6B Oil 6 Gas Journal • Oct. 2J. 199= OCJ SPECIAL r ' <br />^~~~ <br />