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Karbonatne kamnine Pece = Carbonate rocks of Mt. Peca, Slovenia
Bole, Bernarda
Karbonatni masiv Pece gradita wettersteinski apnenec in dolomit v zagrebenskemin grebenskem razvoju ladinijsko-karnijske starosti. Apnenec v zagrebenskem razvoju je plastovit in po strukturi pripada ...intrabiomikritu, intrabiopelmikritu ter loferitu. Nastajal je v plitvem in mirnem sedimentacijskem okolju z občasnimi kratkotrajnimi okopnitvami. Za grebenski facies so značilne korale, alge, spongije in drugi grebenotvorni organizmi. Večji del apnenca Pece je rahlo dolomitiziranega, grebenski del pa je še močno rekristaliziran. Glede na fosilno združbo uvrščamo grebenski apnenec v karnijsko, v glavnem cordevolsko starost.
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