TY - JOUR
T1 - Chemical and Sr-isotopic variations during diagenesis of Miocene siliceous sediments of the Monterey Formation, California
AU - Brueckner, Hannes K.
AU - Snyder, Walter S.
PY - 1985
Y1 - 1985
N2 - The formation preserves siliceous sediments at progressive (generally with depth) diagenetic stages. The chemistry of most diatomite is controlled by three primary phases (biogenic silica, carbonate, and detrital clay) and several subsidiary phases (organic material, apatite, pyrite, and detrital minerals including quartz and plagioclase). -from Authors
AB - The formation preserves siliceous sediments at progressive (generally with depth) diagenetic stages. The chemistry of most diatomite is controlled by three primary phases (biogenic silica, carbonate, and detrital clay) and several subsidiary phases (organic material, apatite, pyrite, and detrital minerals including quartz and plagioclase). -from Authors
UR - http://www.scopus.com/inward/record.url?scp=0022249743&partnerID=8YFLogxK
U2 - 10.1306/212F872E-2B24-11D7-8648000102C1865D
DO - 10.1306/212F872E-2B24-11D7-8648000102C1865D
M3 - Article
AN - SCOPUS:0022249743
SN - 0022-4472
VL - 55
SP - 553
EP - 568
JO - Journal of Sedimentary Petrology
JF - Journal of Sedimentary Petrology
IS - 4
ER -