Stratigraphic Studies Of the Nowshera Reef Complex, Nowshera ...

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42black, fetid, fine-grained limestones, and highly porous dolomites. The combinationof reefs, fetid limestones, and porous dolomites has potential economic,implicationsfor the discovery of oil "(Teichert and Stauffer, 1965, p. 2, and Stauffer, 1968, p. 1349).CONCLUSIONSOn the basis of this investigation the writers conclude that:1. The Kandar Phyllite is the oldest formation exposed in the area, the age ofwhich may be Lower Silurian to Middle Silurian.2. The main reef complex is divisible into three definite layers . These threelayers arc collectively known as the Nowshera Formation:(a) Carbonate Rocks: dark grey to buff coloured limestones with abundantbrachiopods, tabulate corals, and crinoid columns.(b) Reef Core: the central axial region of the reef: mainly spongy cavernouslimestones and dolomites with cavities filled with silt and sand.Characterized by such organisms as massive Favosites, Thamnopora,Cladopora, Mucophyllum, ?Streptelasma, brachiopods, large orthoceroidnautiloid cones, crinoid columns, and large, recrystallized, massive,encrusting Stromatopora.(c) Reef Breccia: a dominantly clastic carbonate rock formed by theaccumulation of organic debris, mainly belonging to Crinoidea, dendroidFavositcs, the fistulosc or dendroid rugose corals Thamnopora and Cladopora,the solitary rugose corals Mucophyllum, ?Streptelasma, Hexagonariaand brachiopods such as Atrypa, Gypidula, Spirigerilla, and Spinella.3. The Misri Banda Quartzite is the youngest formation and was formed bythe deposition of clastic material brought from land. Its textural as well asmineralogical maturity suggests it to have been beach sand.4. The Misri Banda Quartzite is nota sedimentary body of uniform thicknessor a blanket shape, but a lens. It interfingers with the carbonates of the reef.The clastic facies increases towards Misri Banda in the south.5; The age of the Misri Banda Quartzite in this region is probably UpperDevonian.6. The Misri Banda Quartzite Formation can be correlated with the upper partof the Muth Quartzite.7. The purely clastic facies of the Muth Quartzite exposed in Spiti, Kashmir, and~ - ~ ~ -Hazara-tends -to-be come~both~he calcareous (the Nowshera Formation)' and
REEF BRECCIA ._ WIT H AeUNQI,NT FOSSil FRAGMENTS, MAINLY~, DENDROID FAVOSITES, & CRlNOIOAL STEMS,GEOLOGIC.AL MAP OF THE NOWSHERA REEF COMPLEX NO:-1I.,.........~~'CI8ETWI;EH HAWA KILLI e , KANDAR VILLAGEALLUVIUM & lOESSLOCATION MAP,r:::---;;--:---:c- .,.,.,.,.,---NREEF CORE _ MASSIVE COLOMITE & LIMESTONE.WITH ABUNDANTSTRDt.4ATOPORIDS, ~S_ NAUTILOID CONES & OTHERRUGOSE CORALS, MAINLY MUCOPHYLLUM a. STREPTEI ASMA . PELECYPODS& G4STROPOOS IBELLEROPHONTiD l?l GASTROPODS IN PIR SABAK AflEA,CARBONATE ROCI(_ MARLY LINESTONE _WITH ABUNDANT BRACHIOPODS,MAINLY~, ~, .. ~. ~ COLONIES ABUNDANT.~ "'ISRI BANDA QUARTIlfECEI:::J NOWSHERA FORMATiONE=-;::=t=!I:!.T..LT-FIPHYLLITE }KANOAR PHYLLITECRINOIOAL LIMESTONE1_OOLERITE INTRUSIONS1--'"'-'1 CONTACT1-p-1'-3 FAUll~ OP, STRIKE31E E F . B R E C CIAEEFCORER'NAWA KILLIGRAVE YARD/." '1""CARNAnTO HAWA KILll250IISOI
Page 1 and 2: Geol. Bull. Univ. Peshawar, Vol. 4,
Page 3 and 4: 35growth of encrusting organisms li
Page 5 and 6: 37The thickness of the thin-bedded.
Page 7 and 8: 39The Reef Breccia is the uppermost
Page 9: 41(i)Nowshera Deposits.These deposi
Page 13: 43clastic (the Misri Banda Quartzit

Stratigraphic Studies Of the Nowshera Reef Complex, Nowshera ...

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