Page 316 - Carbonate Facies in Geologic History
P. 316
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------------- Oklo LITHOLOGY DOMINANT EVAPORI T E ~ - "'" t ""'"'' CAR80", .. TE 60mites 40 , 20 t a I , ! , I i I I , I 100km SO o sand rim at the edge lime is dashed lines
~~J';s~ J \J / I Basin ~ ,1000 ,=-:,,// black laminated basinal limestone. Area within faint
ES:t~%;y:7J B6NE-~~~J) Texas Fig. X -17. Lithofacies and isopachous map of the Middle Permian San Andres Formation. The El Reno facies is red silt and shale; the sandstone (dotted pattern) is termed Glorieta in northwestern New Mexico; the Blaine is terrigenous sediment and
AN 0 R SPRINGS ES ACI ~
---- ... "" '\ \ , extensive gypsum; the San Andres and Concha Formations are shelf limestones with a is
------------ Mex o N I sA '>,." Eroded southern basins; the Bone Springs facies After Meissner (1972, Fig. 14), courtesy of West Texas Geological Society
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500 500.
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