ML15275A215
| ML15275A215 | |
| Person / Time | |
|---|---|
| Site: | Diablo Canyon  |
| Issue date: | 09/30/2015 |
| From: | Campbell B - No Known Affiliation |
| To: | Rules, Announcements, and Directives Branch |
| References | |
| 80FR37664 00040, NRC-2009-0552 | |
| Download: ML15275A215 (4) | |
Text
UNITED STATES NUCLEAR REGULATORY COMMISSION WASHINGTON, D.C. 2055540001 L;J rO r,..,SUNS! Review Complete Template = ADM -013 E-RIDS= ADM-03 Helium finding adds new wrinkle to Newport-Inglewood fault ermntact the reprter 0 0 WThen Jmm Boles went to the Sattt Fe Spsntgs ott fteld three yecars ago to stndy tsheium samples, he wasntt thsinking ahbett eaethsqtakes.
As a teerelh r in petroestem geology antd geohelttnstrs.
Boles was stdyintg why the temperatures swere so hot untderground lost to he tisoroogh.
he took a fire other sansptes front neath) areas What he fotnod was snrprising And his eesoareh is nose sparking a ness round of debate on the forosattons ot the Neer-poe-lnglessood fnelt. wshieh wras responotiel for one of the most desttnetive earthquakes tn Sotthcrnt Catefonna htstors Boles dtdntf realize ntat the trae, hut some of hins gas sam-pl es followed the path ofthe fault, swhtch outs from Orange County to tho Westusde of Los Astgeles His research showed that helium was leaking deep uedergtroundt theough th fault,.k\ Newport-,,Inglewood
\ \,fault zone Boles said this suggests the Newport-inglessood fault is mush deeper than swhat prevtous studtes shoswed, coneueting sootehos all nay to the Eaeth's umantle."A lot of science is doue by aceident, bet wh4at ste ha e to do is He), there's something tmportasn here that's some out of thins'" sau Boles, professor emeritus at UC Santa Barbata and lead author ofra ness study published in June. "And it has nothisg to do with the original intent" Setsmis exports said the hliumm doesn't ncesaty mean there is a greater quake rtsk on the Nessprt-lnglewood fault Rahe, it higldights just hess much is stidI unknowni about the deepest seettons of the fault.'1'hss ts one step closer to refining mar anderstandtng of the deep structure" of the fault, said the U.S. (Jonia Snevey's Ken Hunt who s, as net involved with the sotuly. "We all live here. in Los Angeles Cosmty, right on top of a whole bunch of active faults, and we're still stuek wtth mferong what the deep structure is. We don't hase clear images" The fault ts about 46 tisles long and is considered patiseslarly hazardous hesause it runs through heavily populated areas, from Culver Ctty through Baldwin Hills, Long Beach atnd Huntington Beach before it heads olffshore.
The fault unleashed the 1933 Long Beach eatthequake, which killed 120 people and promspted some of thte state's firs seismic budlding regulations.
Itfs unclear bosw often large quakes rupture on the fault. In just the taut foss mnaths, the Ncwp~ott-tnglewood fault prmduced sevesa smaill quakes that rattled parts of the regton It's like a pingpong volley between scientific ideas about the deep structure of the Newport-lnglewood fault .... The hope is that you're getting closer to the right answer.- Ken Hdnut US. Geolgica surve The ness fisdings do nut changc the uny scientists forecast quakes along the fault, Hoduat said Experts said they have long heen uncertain about the depth of the Newpcort-nglcscond fault, so corrent earthqu~ake models and ealculations already factor in the possibility of a deeper fault.Boles' studs' analyzed 24 gas samples taken from oil wells along thc fault Unlikc hat spots such as Yelloswstone, where thmree is sorpiug magma that allows heltum to escape to the Earth's sar fant, heltum leakage is unusual for a feature like the Nes3xpot-luglewond faltt+ Here, the fault is squeezing scctions of the Earth's upper emust Ingtbr. which should he lieitinag thc passage of gas flute deep beneath the ground` Boles satd.Heliunm, or more accurately the isotope helium-3, is a vcstige of the big bang and conmes from the Earths's stantle, the layer beneatb the tosser crust, he said. In onler for helium to he escaping from the Newport -Inglewood fautff the fissure must go deep enough throegh the lower crust and connect somebow to thc mantle, said Boles, whose coady was published in the jouroal Geocehesist rv. (lcephvsies, Goosystemss (0-Cubed).The Earth's crust ts at c~ast 30 kitomeses deep. Boles said. Close .nages of the Nesport-Inglensood fault corrently go down only as far as 10 or I) kilometers.
Also interesting, Boles said. ts that he didn't fled just one helium "anomaly" along the fault. Hts tiane ideetified notable amonuts of heltum in areas froma Beverly Hills to Orange Cosunm.Heltum-3 is different than the Ixpe used to blow up baltoouss Although the amounts found wcre sigtuficant for scitonsts.
they would probably go undetected by' anyone passing by.S~eetista iniialty thought the fault soas suimiar to sections of the San Andreas fault -- a so-called strtke-sltp fault dthat cots through the Earth's crust in a retatevety vertical way.
the 198s.b howver. ness studies, mere odf-welt data and better staging techmiques promepted some scienitsts to meconsider what the deepest pasts of the Nevpr-tnglewood fault might took like Ncss theories petnted to the possthttsty that a flatter. shaeste fault cots off the maiu sections of the Newportingiewood fault -- which indicates that the fault might he more shallow and tomss vrtscal than inialtay believed+Studying the spoctfre angles of the fault at such depths ts not earsy, said Hodout of the USGS. The helium flidings suggest that sctsmolngists might want to take ansother look at the original, mlore vertical strike-slip medel ofthe fault 4 S"Its like a pingpong vorley between scientific ideas abont the deep stenetne of the Nemporl-lnglewood faelt," Hadnat sand. 'This t the normal progression of seiene. right? Yen have one paper, and then another paper, and then another paper. And tthnogh time, the hotpe io that younre getin cloe to the ngh anme tiadnat sand there were tstevea elenroents of the study that tinrguste bins. It found that th ameoun of helime leaking from the Newpoer-Inglemood faolt wao greater than mhet osas found in prreeous helimo stadies of the San Androm faeft. The San Andreas fault it slipping apart roughty t0 times foster dman the Nrswpor-higlemood one, so ti mould make more seotse sf there mere mere mantle-derived helium coming ont of the San Andreas, Hodnat sai4 Boles' stady wao eo-aathored by a ream from Tufts Unaivernitry, Occidental Oil & Oat Corp. and NOAA's Pacific Marine Environmental Thre roreareh mas suppoered by NOAA and the U.S.Orparsoren of Energyv's Offlee of Bane Energy. Screnees.Boles, mahe sand be's no qoake expert, said he heoes his team's research leads to mere studies of the fault."It's irke throwing a grenade into the room," be sand, tosalling a colleague's reaction to hin study As for the original Santa Pc Spnsgs sample that promtpted his research rn the first place? Boles fosad nothing unusuol.