Page 207 - Carbonate Facies in Geologic History

..... '-D ~ ~ ::l ::l en '< ~ po ::l 65' ::l t-< ~ (1) ...., "0 (1) a ~f C/) ::l" (1) ::::; ~ e; (JQ s· 'Tj ~ (ii' en

381 PK-GR fUlK WK Tubiphytes
No SVN -SO .- lof'i- backreef with

: RouNDEO I:, : I GR ... INSTONE ' " 1:-,.:;; 18IOCl ... STS, FuSULINIOS ~OOLOMITE TUBULAR FOR .... ~ .OUNOSTONE ~ immediate

MICRITE

WC-I
TUBI PHYTES BOUNOSTONE C'\:i1 PL"'TY "'LGAI.. BRECCI ... TEO

~ ~ ....... EVIIoTED plate development down slope and in

10M "'RE Fig. VI-22. Section across Kemnitz shelf margin Lea County, New Mexico in Lower Wolfcampian interval indicated on section in Fig. VI-21. Line of boundstone and rounded bioclastic grainstone at shelf margin. Conglomerates are interbedded in slope deposits and mark two breaks in deposition

SPIC
X10 algal
FLNK

400 M P ... CKSTONE, GR ... INSTONE, W"'CKESTONE, FL ..... K KOS, SPICULITE WI( Petrographic study indicates

GR
on Fig. VI-23.
PI(

CONGL~' spICI",;~ 10,858
So WO-I .. 1 indicated within and at top of buildup

section
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