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11 <br />DAUB b ASSOCIATES _ +~. \ry ._,, <br />CONSULTING GEOLOGISTS _ -~ ~'.',~I+Zry"+::~~ 1980 fi0U1H BROAOWav <br />}~:=+j~r::..S ..~;:I :.+~,~'-•.`h"r.';'~l~~n'. .,.. P~•yi ...~....: .,. -.; ... GRAND JU NG~ION. CO BI503~9593 <br />. .. .~ 1]O]I 2a 1 096 <br />~{_ ! Reed=n{ Pr{h_ 1 Bant_ a Covent{ <br />A-IT i_5,1 <br />4-3 4.1.1 <br />4-5 9.2.2.2 <br />N <br />b <br />4-5 4.2.2.2 <br />4-6 4.2.2.2 <br />{-5 4.2.2.2 <br /> rp}] pb ova thepa Qrp}ep{ap !pQ flip <br /> goi loep}eQ op or gapr !gp 60 <br /> flopQp3p}pe <br /> - <br />, <br /> xheo roe ie k eoouE dornsire u, <br />~ <br />s I2. <br /> c <br />? <br />whet •treer <br />ere you referring tJ 49 <br />SD I horeve r, there rill ¢p • potential <br /> for ... <br />1 6 The rock goal lty of the •ejority <br /> of the strati{reDhlc section eb ova <br /> the dissolution surface 1• elreedy <br /> very poor. <br /> Reaove to the Mehe[evy sane. 'the yg <br /> Mehogeny cone hea very poor rock <br /> quel~ty iv part. This fe elreedy <br /> stated by referring to the <br /> •ejority. <br />1 7 ... effect rock quality of the <br /> overlying etrete tgedlptely <br /> orerliiv{ the ceylt=_ <br />2 6 on the rock quality of the <br /> Mehogeny sons beceuee of cevin(. <br /> Aeek pus}iti 1n_ the loypr lapghed <br /> Sons is elrepdi v_pr= peor pad vo y~ <br /> reel pd v_erae ~ppest could Sep p}t <br /> to the roclj thfou{y th}p <br /> ptSptl{Sephle lvtervpl_ <br />4 2 et the CoD• of the pills rs. <br /> Bfeee the tap of the plllerp ere <br /> in_ op¢co_1 }tam the ciuph~v{ of <br /> there plllerp woo}~ Sepppble ppi4 49 <br /> of p pleptte flat due to the <br /> vptu_iy of jgp pps5p~}t:. <br /> Ther< is vo need to include the <br />11 <br />ii <br />DAUB b ASSOCIATES <br />CONSULTING GEOLOGISTS -i~l'I ~~'.i+]'~t9/' ~Z ••,;, <br />' ~~~' ~<' _..; ~K ~. 1980 SOUTH BROADWAY <br />:v~ .. . ;. :. n <br />"~~~~'~T ~~D'u~.~~~+f. ~•~%~iI^cp ~1'r, .J ~~l~'+~t. ~, ~:'l~..•-.^. GRAND JUNCTIO N, CO B150]~959J <br />~~ ~~ ~ ~ ~ IJ0312a 4096A <br />P{_ a ~eedln{ PS{h_ 1 Sae t_ I Coppente <br />cord ((allure) So the precedln[ <br />•entevice. <br />{-5 q,2.2.2 9 7 overt ylnf the cavil(<s uD !.^.~^ 49 <br />}49 SRSS pooS Tpsk pRldl}S pf F¢: <br />}ppf994 {pgp• J <br />4-7 4,3.1 2 2 It Ss herd to conceive that the <br />borehole >,ey be loot end that the <br />•ived out tevitle• could not be <br />drilled throu[h. Natural 1$ <br />•ube idence end vgfy poor rock <br />quality i• ellerdy prevalent with <br />note rv ua vojdl trot the netu rat <br />d ieeol utlaU+ef saline •Lnerels. <br />4-8 q.3.2.2 1 3 To ensure that there were no open <br />voids left ocrosa the Mehogeny <br />cone, the egtira pace woo}Q ¢p <br />plu{{ed upon well ebegdenpegt. <br />the sentence would reed better end <br />ie tore eecurete. There [• no <br />reel potential for gee to <br />eccusulete ecroa• thi• interval. <br />No ge• hea ever been detected in <br />the Parachute Creek •esber until j <br />the saline zone hea been $ <br />penetrated. The leeched cone (R- <br />8 to the diesolutlov •ur Pe <e) 1• <br />vch too De rr eeb le end Do rou• to <br />allow the a<curuletion of <br />•i[nititent erounts of natural <br />[es. The abandoned well will <br />contain s corpet<nt plug{in{ {el. <br />Carent across this interval L• not <br />e nec eaeity end plu{[in{ gel le <br />core [hen adequate. <br />4-e q,3.2.2 2 8 Sodiur resources within ppi} of <br />the L-56 bed could also ... yg <br />Only Dert of L-5p bed could be <br />12 <br />