[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"doc-detail-228348-en":3,"doc-seo-228348-105":29,"detail-sidebar-cat-0-en-105":95},{"code":4,"msg":5,"data":6},0,"success",{"doc_id":7,"user_id":8,"nickname":9,"user_avatar":10,"doc_module":4,"category_id":11,"category_name":12,"doc_title":13,"doc_description":14,"doc_content":15,"file_id":16,"file_url":17,"file_type":18,"file_size":19,"view_count":20,"is_deleted":4,"is_public":20,"is_downloadable":20,"audit_status":20,"page_count":20,"language":21,"language_code":22,"site_id":23,"html_lang":22,"table_of_contents":24,"faqs":25,"seo_title":26,"seo_description":14,"update_tm":27,"read_time":28},228348,24189269381491,"Bill Black","https://ap-avatar.wpscdn.com/avatar/160000cf11732dd8392?x-image-process=image/resize,m_fixed,w_180,h_180&k=1788146458752108895",8,"Research & Report","CORRELATION OF MAP UNITS - Geological Map Analysis","Correlation of map units for the Ketchikan and Prince Rupert quadrangles, Alaska, using atomic-absorption analysis of stream-sediment samples and related geochemical methods. The document outlines how analytical values were grouped into four ranges represented by different symbols, explaining variability caused by lithology, sampling practice, analytical variance, and chemical weathering. Reference publications and reported analytical datasets support sampling sites, station coordinates, scale details, and interpretation of bedrock mineralization likelihood while noting limitations for single-element anomalies.","13c  \nCORRELATION OF MAP UNITS  \n\n| Tep  \u003Cbr>Tkp  \u003Cbr>TKP  \u003Cbr>户  \u003Cbr>MA\"  \u003Cbr>TK  \u003Cbr>4气  \u003Cbr>而  \u003Cbr>Ne  \u003Cbr>·0  \u003Cbr>THp  \u003Cbr>MR.  \u003Cbr>匠  \u003Cbr>应  \u003Cbr>M他u  \u003Cbr>M丹  \u003Cbr>M9g  \u003Cbr>T  \u003Cbr>P  \u003Cbr>0  \u003Cbr>M  \u003Cbr>fzB4  \u003Cbr>T网  \u003Cbr>0  \u003Cbr>M:A  \u003Cbr>险  \u003Cbr>R  \u003Cbr>eU  \u003Cbr>8-4  \u003Cbr>TR  \u003Cbr>sn2o  \u003Cbr>有3  \u003Cbr>rBp  \u003Cbr>你  \u003Cbr>4s  \u003Cbr>AV  \u003Cbr>GT  \u003Cbr>A  \u003Cbr>Aiv  \u003Cbr>LA  \u003Cbr>KJg  \u003Cbr>int  \u003Cbr>K  \u003Cbr>3  \u003Cbr>M丹中  \u003Cbr>:  \u003Cbr>H  \u003Cbr>R√  \u003Cbr>H  \u003Cbr>up  \u003Cbr>Te  \u003Cbr>Ha  \u003Cbr>0  \u003Cbr>KJs  \u003Cbr>BJL  \u003Cbr>个  \u003Cbr>M校a  \u003Cbr>7a  \u003Cbr>H  \u003Cbr>Jv  \u003Cbr>4  \u003Cbr>P  \u003Cbr>116  \u003Cbr>A  \u003Cbr>p  \u003Cbr>k.  \u003Cbr>十应  \u003Cbr>Bp  \u003Cbr>F  \u003Cbr>z  \u003Cbr>4  \u003Cbr>og  \u003Cbr>国丹  \u003Cbr>t  \u003Cbr>pu  \u003Cbr>R  \u003Cbr>o Wale  \u003Cbr>KJ:  \u003Cbr>十  \u003Cbr>PkAp  \u003Cbr>K  \u003Cbr>1  \u003Cbr>Hz作  \u003Cbr>a  \u003Cbr>Rp  \u003Cbr>Rv  \u003Cbr>四  \u003Cbr>esi  \u003Cbr>O  \u003Cbr>M及u  \u003Cbr>Mu  \u003Cbr>Ix  \u003Cbr>Penr  \u003Cbr>MF  \u003Cbr>m  \u003Cbr>bland  \u003Cbr>8  \u003Cbr>Ku  \u003Cbr>0  \u003Cbr>N A T  N  \u003Cbr>亿u  \u003Cbr>HA  \u003Cbr>P  \u003Cbr>n  \u003Cbr>Tan8  \u003Cbr>P  \u003Cbr>刀d  \u003Cbr>地Ap  \u003Cbr>马  \u003Cbr>阜  \u003Cbr>C  \u003Cbr>M:  \u003Cbr>81e  \u003Cbr>望  \u003Cbr>bsland  \u003Cbr>r  \u003Cbr>u  \u003Cbr>作p  \u003Cbr>ub  \u003Cbr>Y  \u003Cbr>Tn  \u003Cbr>1u  \u003Cbr>So  \u003Cbr>5N,T  \u003Cbr>n  T  \u003Cbr>AA  \u003Cbr>AL.  \u003Cbr>TTH 4LTS  \u003Cbr>pe  \u003Cbr>罪  \u003Cbr>的  \u003Cbr>F  \u003Cbr>pUNDAS  \u003Cbr>r点e8a23  \u003Cbr>1s/LAVD   |\n| --- |\n\n[Geolagic m&p generalized [rom Berg and others(1978]uGTEFN2=72L.ATEFN4RY7TTnpMiocena  \nTepEc=4n1EPTI9Y  \nTEATIAEY CRTKpCRETG亡EDu9KJuNET&CEUSK&5KJY1URESSIC3UFA35C ORTAIa9S1CTSW}Upar YriasleTRIAssic  \nMESDZCMC CRM7Rp   :PAL[czCICW ndle =zxP  \nDRFzpSilurinnCLDERPZ婴  \n[ESCRIPT1CN CF YAP LK[TS  \nLSDCHSCLIDMTED DEPKSZTS,LOTVTDED ICuatcrrarlLCAMIC S85 CuaLie ury anl TerLiarylheUnE[VIEED PICC[M L₁T0%1E 0xsTepUMDLVZDED EDCE.E PLUTCMIC RDC格TKpIETVCF TERT[Y CAETA2E0LS PLUTDNE SCDRS  \n望1 TSL GM FPNT[09 AH IBMn 0R5FtATIVY 85 (er CrebatP:s nr llper Lrisslt:)UI trzn1c ard other plutznic YccksMetasedircntary fucksMeLiwlnic ruuks  \n\n| KJup   |\n| --- |\n\n\n| J   |\n| --- |\n| kLIv   |\n\nTXAS CE GPAnULURLIL (Jzress c ur friessie!METAMCRF5LD YULCEC AHD SEDLNENTRY RCCIS〔Lurassic cr Triessic〕MTPMCHP-DSE SEDTPENT5Y A 73L2NTC RCCIS〔Lper Trlassfc〕DARAEISS D HPHTFCL1TE (sz0it or   uoic)ET3MCRGC 808S,1CTWIDD Nestzit or Poleszoic)  \n\n| I+   |\n| --- |\n| 1Bv   |\n\n\n| 8v   |\n| --- |\n\n\n| zp   |\n| --- |\n| 生   |\n| 隐用   |\n| 15,   |\n|  |\n\nMETAHRFHSE SEDIENT65Y   阳MG 70LCNIC RDC(H1dcle and upper Faleozcic;FELSIL ETCLDNID RCCS Iale:z0c Dr c1cer)PLIT的SDx5,CHEFLY TSWHIFPITE (Siluriait ar il rlar)METAMPPHSB)SFINAT期AY A 00CATE自2S 151lurlas er uiderSTUULS  \n\n| F2s%   |\n| --- |\n\n……Ccntact.hpproxia te iy located;dotted nhere curceelet….High-angia fault.  eshed where inferresl;dotad sher mealedTr rusl.fau1t..Ched whare cDHceslac,fBfeered,aP assLred5anteeth cn upper plete  \nTase fron DSGS 1:280,00U topo sertes;  \nGeolocy by H.Ber,R.Carten,J.Ch11ds,A.Clark,  \nH.Cordcn,N.C1ogles,G.Dunme,R.E111ott.  \nKETCPJRAF,1955;PRINCE RLPERT,1959.  \nC.iol1cnay,J.oLqhtan,R.Koch,R.Miller,  \nALASKA-CHNODA.  \nR.Rudser,1.Sith,B.Wiggins,1956-1977  \nDATP上ERL 20FEET  \n风IL NLEN SA LŁ.  \nPF0CINAE HEN  \nCELLIhATCK,1455  \nMAP SHOWING COPPER DETERMINED BY ATOMIC ABSORPTION IN STREAM SEDIMENTS,KETCHIKAN AND PRINCE RUPERT QUADRANGLES,ALASKA  \n78-73 C  \nKoch and othera--0eochemistry -Cu  \nIn the ccurse cf U.5.Ge:looica1 Survey inivgstigations Df the Ketch iken andPrince Rupert quadrangles,2602 stream-sed-ment samples were cc1ected.Sarl-ples Mere analyzed fay up to 3C elements by a 6-step,seniquant1tative emfs-sim spectrnsrnpir methnd(Gr ines and Narranzino,1958}and foru ta 5 ele-ents by a tanic-alsarptian sperctrophatometry(s rd and others,1959).ThisTMi shcus sanple!colnction sites fow 2321 samplos which urre analyzed forropper hy the atomic-a5soption method.Complete ana!yticl data plus loticn maps(scale 1:125,000}.station coordtnates,and a d¹scussion o7 samp?inganalytical orocedures for 5anples frcm s1 tes shT cn this nap are pub11shed1n Lwu reports (Kech and E7Tiott,1978b,c).These data are also ave11ablen magnet1c coTputer tape(Kach,Yan Tninp,and N Dana1,197E).  \nBarkgrnund leve1s vary for different litholcgies and in differnt areas.  -Cause nf this and variahility introduced from ","cbCain0et44IcqG6","https://ap.wps.com/l/cbCain0et44IcqG6","pdf",3839785,1,"English","en",105,"# Correlation of Map Units\n## Geochemical Data and Analytical Grouping\n## Sampling, Reporting, and References","[{\"question\":\"What analytical method is emphasized for the copper determinations?\",\"answer\":\"Copper is determined in stream sediments using the atomic-absorption method, with samples analyzed by multi-step semiquantitative and spectrophotometric approaches before being finalized for atomic-absorption analysis.\"},{\"question\":\"Why are analytical values grouped into ranges with symbols?\",\"answer\":\"To manage variability and support generalized interpretation, since levels vary by lithology and region due to sampling practice, analytical variance, and chemical weathering. Single-element anomalies may not be reliable without neighboring support.\"},{\"question\":\"What information is included with the published analytical datasets?\",\"answer\":\"Complete analytical data and listing maps, including scale information, station coordinates, and discussion of sampling and analytical procedures, along with availability of additional data via magnetic computer tape.\"}]","CORRELATION OF MAP UNITS - Geological Map Analysis | PDF",1789025074,3,{"code":4,"msg":30,"data":31},"ok",{"site_id":23,"language":22,"slug":32,"title":13,"keywords":33,"description":14,"schema_data":34,"social_meta":90,"head_meta":92,"extra_data":94,"updated_unix":27},"correlation-of-map-units-geological-map-analysis","",{"@graph":35,"@context":89},[36,52,72],{"@type":37,"itemListElement":38},"BreadcrumbList",[39,43,47,49],{"item":40,"name":41,"@type":42,"position":20},"https://docshare.wps.com","Home","ListItem",{"item":44,"name":45,"@type":42,"position":46},"https://docshare.wps.com/document/","Document",2,{"item":48,"name":12,"@type":42,"position":28},"https://docshare.wps.com/document/research-report/",{"item":50,"name":13,"@type":42,"position":51},"https://docshare.wps.com/document/correlation-of-map-units-geological-map-analysis/228348/",4,{"url":50,"name":13,"@type":53,"image":54,"author":59,"headline":13,"publisher":61,"fileFormat":64,"inLanguage":22,"description":14,"dateModified":65,"datePublished":66,"encodingFormat":64,"isAccessibleForFree":67,"interactionStatistic":68},"DigitalDocument",{"url":55,"@type":56,"width":57,"height":58},"https://docshare.wps.com/thumbnails/correlation-of-map-units-geological-map-analysis/228348.png","ImageObject",300,407,{"name":9,"@type":60},"Person",{"url":40,"name":62,"@type":63},"DocShare","Organization","application/pdf","2026-09-11","2026-09-10",true,{"@type":69,"interactionType":70,"userInteractionCount":20},"InteractionCounter",{"@type":71},"ViewAction",{"@type":73,"mainEntity":74},"FAQPage",[75,81,85],{"name":76,"@type":77,"acceptedAnswer":78},"What analytical method is emphasized for the copper determinations?","Question",{"text":79,"@type":80},"Copper is determined in stream sediments using the atomic-absorption method, with samples analyzed by multi-step semiquantitative and spectrophotometric approaches before being finalized for atomic-absorption analysis.","Answer",{"name":82,"@type":77,"acceptedAnswer":83},"Why are analytical values grouped into ranges with symbols?",{"text":84,"@type":80},"To manage variability and support generalized interpretation, since levels vary by lithology and region due to sampling practice, analytical variance, and chemical weathering. Single-element anomalies may not be reliable without neighboring support.",{"name":86,"@type":77,"acceptedAnswer":87},"What information is included with the published analytical datasets?",{"text":88,"@type":80},"Complete analytical data and listing maps, including scale information, station coordinates, and discussion of sampling and analytical procedures, along with availability of additional data via magnetic computer tape.","https://schema.org",{"og:url":50,"og:type":91,"og:title":13,"og:site_name":62,"og:description":14},"article",{"robots":93,"canonical":50},"index,follow",{"doc_id":7,"site_id":23},{"code":4,"msg":5,"data":96},[97,101,105,109,114,119,124,127,132,135,139],{"id":20,"doc_module":4,"doc_module_name":45,"category_name":98,"show_sort_weight":99,"slug":100},"Story & Novel",90,"story-novel",{"id":46,"doc_module":4,"doc_module_name":45,"category_name":102,"show_sort_weight":103,"slug":104},"Literature",80,"literature",{"id":51,"doc_module":4,"doc_module_name":45,"category_name":106,"show_sort_weight":107,"slug":108},"Exam",70,"exam",{"id":110,"doc_module":4,"doc_module_name":45,"category_name":111,"show_sort_weight":112,"slug":113},5,"Comic",60,"comic",{"id":115,"doc_module":4,"doc_module_name":45,"category_name":116,"show_sort_weight":117,"slug":118},6,"Technology",50,"technology",{"id":120,"doc_module":4,"doc_module_name":45,"category_name":121,"show_sort_weight":122,"slug":123},7,"Healthcare",40,"healthcare",{"id":11,"doc_module":4,"doc_module_name":45,"category_name":12,"show_sort_weight":125,"slug":126},30,"research-report",{"id":128,"doc_module":4,"doc_module_name":45,"category_name":129,"show_sort_weight":130,"slug":131},9,"Religion & Spirituality",20,"religion-spirituality",{"id":130,"doc_module":4,"doc_module_name":45,"category_name":133,"show_sort_weight":130,"slug":134},"World Cup","world-cup",{"id":136,"doc_module":4,"doc_module_name":45,"category_name":137,"show_sort_weight":136,"slug":138},10,"Lifestyle","lifestyle",{"id":140,"doc_module":4,"doc_module_name":45,"category_name":141,"show_sort_weight":110,"slug":142},19,"General","general"]