Copyright © 1979 Ohio Acad. Sci. 0030-0950/79/0001-0024$! .50/0 DESCRIPTIVE MINERALOGY OF PUGH QUARRY, NORTHWESTERN OHIO: CALCITE, DOLOMITE AND FLUORITE1 DAVID F. PARR2 and LUKE L. Y. CHANG, Department of Geology, Miami University, Oxford, OH 45056 Abstract. Calcite is by far the most abundant mineral in the Devonian rocks at Pugh Quarry. The large crystals, from 5 mm to 10-15 cm long, are predominantly brown with wide variations in hue and intensity. The small crystals, smaller than 5 mm, range from colorless to gray-yellow to pale yellow. Both large and small crystals consist almost entirely of scalenohedral forms (dog-tooth spar habit). The most common and most easily recognized type of twinning in the large crystals is on the (0001) plane. Both dolomite and fluorite are minor minerals at Pugh Quarry, al- though fiuorite is found in all parts of the Quarry. Dolomite crystals occur as second- ary encrusting material and are most common in vugs. OHIO J. SCI. 79(1): 24, 1979 In this third paper on the mineralogy crystals were attached directly to the of Pugh Quarry, calcite, dolomite and dolostone with no material in between fluorite are described. The quarry is (fig. 1). In some cases, however, ran- located in the SW3^, SW^, Sec. 6, domly oriented, anhedral grains of cal- T.4N, R.9E in Milton Township, Wood Co., Ohio. Its sulfide mineralization, in- cluding marcasite, pyrite, and sphalerite has been previously described (Parr and Change 1977, 1978). CALCITE Calcite was by far the most abundant mineral in the Devonian rocks at Pugh Quarry. Based on crystal size, calcite could be divided into two distinct groups; large crystals (maximum dimension >5 mm) and small crystals (maximum di- mension <5 mm). LARGE CALCITE CRYSTAL Large crystals were most abundant in the eastern portion of the north wall of the quarry where cavities and collapse breccias are common. Relation to Host Rock. Examination of thin sections across critical crystal-matrix interfaces revealed no evidence of replace- ment activity. Commonly the large 1Manuscript received 19 January 1978 and in FIGURE 1. Thin section, one nicol. Large revised form 4 August 1978 (#78-6). calcite crystals on dolostone. Note the 2Present Address: Department of Geology, lack of any substance separating the body Wisconsin State University, Superior, WI of the large crystal from the dolostone 54880. (arrow). X25. 21 Ohio J. Sci. PUGH QUARRY MINERALOGY 25 cite were located between the crystals and apparently was affected by included the dolostone host rock (fig. 2). Large hydrocarbon material. Higher concen- calcite crystals also have developed on trations of this material, zonally arranged, marcasite and sphalerite crystals. How- produced darker brown bands within the ever, there is no strong evidence suggest- crystals. When cleavage fragments large ing over crystallization of the older mar- enough to show this feature were heated, casite-sphalerite by the younger large the brown color disappeared completely, calcite crystals. Although fragments of leaving the fragments colorless and highly marcaiste were included in the basal por- fractured. When cleavage sections were tions of a few large calcite crystals, the examined under ultraviolet light, the marcasite crystals appeared to be clastic darker brown bands fluoresced a weak particles derived from collapse reecciation dull red color under long wave ultra- of the dolostone which preceded calcite violet light, yet the same areas fluoresced crystal formation. a strong orange color under short wave light. After illumination by either long or short wave ultraviolet light, the outer one to two millimeters of the crystals showed a weak cream to greenish white phosphorescence which lasted only about 7 seconds. No phosphorescence of the darker brown bands was observed. Fluid inclusions were observed in many thin sections. There was no apparent correlation between the abundance of the fluid inclusions and the darker brown , bands. Size. Large calcite crystals were de- fined as being longer than 5 mm along the c-axis. Crystals in the 10 to 15 cm length range were not uncommon (fig. 3). Several large crystals had cleaved nat- urally and had been displaced along or perpendicular to cleavage planes (fig. 4). The surfaces exposed by the cleavage of the crystals had been healed by subse- quent growth of calcite onto the cleavage surfaces. Habit and Form. The crystal habit FIGURE 2. Thin section, crossed nicols. was restricted to the dog-toothed spar Large calcite on dolostone. Note the layer type, common to calcite from many of anhedral calcite separating the body of the large crystal from the dolostone (ar- localities. The crystal faces consisted row). X25. almost entirely of scalenohedral forms modified by the development of numerous vicinal faces. Doubly terminated and Color. The crystals were predomi- twinned crystals were common (figs. 3 and nantly brown but with wide variations in 5), many of these had multiple termina- hue and intensity. The color, as ob- tions resulting from extensive parallel and served on crystal faces and cleavage sur- subparallel growth (fig. 6). faces, was a blend of several internal Forms on the large calcite crystals zones and appeared darker than the could not be determined using an optical overall color. The color and zonation of goniometer or even a contact goniometer color was most readily seen on cleavage because of the large size of the crystals surfaces or on sections of crystals cut and the curved, rough, and dull character perpendicular to the c-axis. The opacity of the crystal faces. varied from translucent to transparent. Twinning. The most common and The overall color of the large crystals most easily recognized type of twinning 26 D. F. PARR AND L. L. Y. CHANG Vol. 79 FIGURE 3. Large calcite-dog-tooth crystals. Note parallel growth and multiple terminations on the crystal. X0.3. FIGURE 4. Large calcite crystal, dog-tooth habit. These crystals have been broken and dis- placed along cleavage planes (arrows). Subsequent calcite growth has covered the cleavage sur- faces with numerous smaller terminations showing distorted growth and many vicinal faces. X0.5. FIGURE 5. Twinned large calcite crystal, dog-tooth habit. The "straight line" contact between the northern and southern hemipshere crystal forms can be seen. Note the dark material included near the crystal surface. Xl.2. FIGURE 6. Large calcite crystal, dog-tooth habit. Note multiple terminations of the crystals and extensive parallel growth. Xl-2. Ohio J. Sci. PUGH QUARRY MINERALOGY 27 present in the large calcite crystals was SMALL CALCITE CRYSTAL on the (0001) plane. Equatorial girdles Calcite crystals included in this group of the twinned crystals were characterized were by far the most abundant and by reentrant angles on alternate corners widely distributed in the quarry. The of the 6-sided crystals. The contacts be- small crystals occurred in the mineral tween northern and southern hemipshere zone of the Anderson dolomite (Parr and forms on the twinned crystals resulted in Chang 1977) throughout the quarry as the formation of morphological zones, the well as in small cavities in the overlying axes of which lie in the (0001) plane and Dundee limestones. were perpendicular to the c-axis of the Relation to Host Rock. Small calcite crystal (fig. 5). crystals encrusted both the dolostone Etching of {0111} cleavage surfaces host rock and earlier formed minerals. showed 6 wedge shaped sections, each of The encrustations were relatively thin, roughly equal area. The sectors were being no more than 3 to 4 mm thick. distinguishable from one another by dif- Examination of thin sections recealed ferent reflectance in their etched surface that randomly oriented, ahedral calcite (fig. 7). Each sector was separated from crystals projected into the open space the adjacent sector by lines which con- (fig. 8). In addition, small calcite crys- nected opposing interfacial angles formed tals served as filling material in the in- by the scalenohedral faces. The etch terstitial spaces in the dolostone. properties of the sectors indicated that Color. The small crystals ranged from opposing sectors were in similar orienta- colorless to gray-yellow to pale yellow. tion. Thus, the 6 sectors may be repre- A minimal pale yellow fluorescence and a sented as 3 pairs of similar sectors (fig. 7). cream white phosphorescence were ob- served when small crystals were ex- amined under both short and long wave ultraviolet light. The phosphorescence was extremly weak and short-lived; de- tectable for only a few seconds. Habit and Form. The dog-tooth (sca- lenohedral) crystal habit of the small calcite crystals was remarkably uniform throughout the quarry (fig. 9). The rounding off of alternate interfacial edges between the scalenohedral faces was pre- dominant, but this modification did not affect the overall dog-tooth appearance. Attempts to determine the interfacial angles of forms failed because the sur- faces of the crystals had been naturally etched to a such degree that reflectivity became very poor. Relation to Other Minerals. Small cal- cite crystals were thinly scattered over FIGURE 7. Polished and etched cleavage sec- marcasite surfaces (fig. 10), and also over tion of large calcite crystal. Six sectors are fluorite crystals (figs. 11 and 12). When visible. The similarity of opposing sections the small calcite crystals were found in can be seen. Xl.9. association with barite mineralization, small spherulites of barite were commonly The twinning was restricted to the in- completely or partially enclosed in the terior portion of the crystals, as the outer small calcite crystals. Barite crystal margins of the crystals, which have been clusters were also found perched on the previously described as the zone of small calcite crystals (fig. 9). This re- phosphorescence, did not show the diag- lationship indicated that these two min- notic etch features.