{"refrec":{"BRefID":368634,"RR":"<b>Galliher, E.W.</b> (1935). Geology of glauconite. <i>Bulletin of the American Association of Petroleum Geologists 19(11)</i>: 1569-1601","BEntID":366360,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Bulletin of the American Association of Petroleum Geologists 19(11)</i>: 1569-1601","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Galliher, E.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Galliher, E.W.","Englishabstract":"Throughout the sediments in Monterey Bay, an area of more than 250 square miles, there is conclusive evidence that biotite alters to glauconite, the genesis of which has been in question for more than a century. By analogy with what is known about sedimentation in the bay, a set of facts is presented which explains the occurrence of glauconite throughout the present ocean basins and the sedimentary column. 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