{"refrec":{"BRefID":368642,"RR":"<b>Galliher, E</b> (1939). Biotite-glauconite transformation and associated minerals, <b><i>in</i></b>: Trask, P.D. <i>Recent marine sediments: A symposium. SEPM Special Publication,</i> 4: pp. 513-515. <a href=\"https://dx.doi.org/10.1306/sv10340c28\" target=\"_blank\">https://dx.doi.org/10.1306/sv10340c28</a>","BEntID":366368,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":", <b><i>in</i></b>: Trask, P.D. <i>Recent marine sediments: A symposium. SEPM Special Publication,</i> 4: pp. 513-515. <a href=\"https://dx.doi.org/10.1306/sv10340c28\" target=\"_blank\">https://dx.doi.org/10.1306/sv10340c28</a>","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Galliher, E","OrigTitleTranslFlag":0,"Authorstringtrunc":"Galliher, E","Englishabstract":"In examining a number of glauconitic sediments, a surprising amount of evidence is found tying glauconite to a biotite or iron-mica derivation. Principal evidence for relationship lies in series of transition grains demonstrating gradual change from mica to glauconite. A most interesting group has been illustrated before (3, p. 1584), but is shown here again since it constitutes one of the best examples from recent sediments (Fig. 1).<p>Groups similar to it have been found in glauconitic sediments collected from about one hundred localities spread over a dozen states and countries. They are not limited to recent material alone, but range down the column as low as Cambrian. Several illustrations of such fossil biotite-glauconite associations are in preparation.<p><p>In addition to individual grains which show the transformation proccess, another line of evidence for the biotite-glauconite relationship is the change in facies in some shelf sediments. By change in facies is meant the gradual change from biotite-rich sands fairly near shore to mixed glauconite-mica silty sands farther off shore and a little deeper, thence progressively to glauconite muds at a depth of about 100-fathoms. A map and description of this type of occurrence in Monterey Bay have been given (2, p. 1354; 3, p. 1570).</p><p>The most potent evidence that indicates intimate relationship of the minerals however, is Gruner’s X-ray work (5). Gruner, in addition to presenting experimental data, gives an interesting discussion and comparison of ionic arrangement and structure of unit cells and concludes that glauconite is a mica in structure (p. 699).","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"Biotite-glauconite transformation and associated minerals","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1939,"MonPub":null,"DateUpdate":"2023-11-13","DateCreate":"2023-11-13","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0,"DOI":"10.1306/sv10340c28"},"refs":null,"anarec":{"AnaID":368642,"PubliDate":1939,"Pagination":"513-515","XtraPublOfAnaID":null,"ISBN":"9781629812519","Volume":"4","Issue":null,"BRefMon":368640,"BRefMonRR":"<b>Trask, P.D.</b> (1939). Recent marine sediments: A symposium. <i>SEPM Special Publication</i>, 4. American Association of Petroleum Geologists: Tulsa. ISBN 9781629812519. vi, 736 pp. <a href=\"https://dx.doi.org/10.1306/sv10340\" target=\"_blank\">https://dx.doi.org/10.1306/sv10340</a>","BRefXtra":null,"BRefXtraRR":null,"SerBRefID":114929,"SerRR":"SEPM Special Publication. Society of Economic Paleontologists and Mineralogists (SEPM): USA.  ISSN 1060-071X","StandardTitleSer":"SEPM Special Publication","ISSN":"1060-071X","AbbrevSer":"SEPM Special Publication","StandardTitleMon":"Recent marine sediments: A symposium","StartPage":513,"Pages":3,"ToPubliDate":null,"BRefBibLvlCode":"MS","SerNotes":null,"AutString":"Trask, P.D."},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Galliher","Firstname":"Edgar Wayne","Initials":"E","Affiliation":null,"Discriminator":null,"CorporateFlag":0,"BEntID":366368,"AutID":544950,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":null,"BEntPrivate":null,"availability":[{"BInstID":393916,"LibID":36,"BRefID":368642,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":null,"ShelfLocCode":"393916","RFID":null,"PaidValue":null,"Medium":"Server","Description":"Interne VLIZ documenten","Acronym":"VLIZ","Library":"Vlaams Instituut voor de Zee","DutchTerm":"Non-open access","URL":null,"ClassifID":228,"Classification":"Non-open access","ReqLink":1,"ClassifTypID":3,"URLLocation":"https://www.vliz.be/imisdocs/publications/","SubDir":1,"InternalReq":1,"LoggedInReq":1,"Disclaimer":"Disclaimer_VLIZ_Intern","DutchDisclaimer":"<p>Deze publicatie is enkel beschikbaar voor persoonlijk gebruik binnen de Innovocean site <br />en mag op geen enkele manier verder worden verspreid.</p>","FileFormat":".pdf","FileDescr":"pdf","InsPub":1,"InsID":36,"FileFormID":6,"LendableFlag":1,"PublicFlag":1,"orderLib":"A","Notes":null,"AccConID":null,"AccessConstraint":null,"LicURL":null}],"litstyles":null,"thespers":null,"arch2discl":null,"SERpubls":null,"MONpubls":[{"PublName":"American Association of Petroleum Geologists","Place":"Tulsa"}],"pictures":[],"thestermsPath":null,"thestermsASFA":null,"taxtermsASFA":null,"geotermsASFA":null,"collections":null,"conf":null,"proj":null,"Physdatasets":null,"spcols":null,"doi":null,"publs":null,"serparttypes":null,"monauthors":[{"AutName":"Trask","Initials":"P.D.","CorporateFlag":0,"BEntID":366366,"AutID":544942,"OrderNr":1,"DegrID":null,"EditorFlag":1,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"AutStrTrunc":"Trask, P.D."}],"MParts":null,"SParts":null,"hLibs":null,"langs":[{"BEntID":366368,"AbstractFlag":0,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"},{"BEntID":366368,"AbstractFlag":1,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"}],"urls":[{"URL":"https://dx.doi.org/10.1306/sv10340c28","externalID":"10.1306/sv10340c28","URLTypeCode":"DOI","URLID":120915,"URLTypID":13,"URLType":"DOI","URLPrefix":"http://dx.doi.org/"}],"thesterms":null,"taxterms":null,"geoterms":null,"othterms":null,"asfacodes":null,"asfa2codes":null,"thestermsFRIS":null,"taxtermsFRIS":null,"geotermsFRIS":null,"othtermsFRIS":null,"resmessage":"","complete":1,"sessions":{"newSesName":"Chisala, Chilekwa, C.","newSesDate":{"date":"2023-11-13 08:07:38.263000","timezone_type":3,"timezone":"Europe/Brussels"},"updSesName":"Chisala, Chilekwa, C.","updSesDate":{"date":"2023-11-13 08:07:38.263000","timezone_type":3,"timezone":"Europe/Brussels"}}}