Knowledge (XXG)

Cerro Aspero Batholith

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Pinotti, L.P.; Coniglio, J.E.; Esparza, A.M.; D'Eramo, F.J.; Llambías, E.J. (2002). "Nearly circular plutons emplaced by stoping at shallow crustal levels, Cerro Aspero batholith, Sierras Pampeanas de Córdoba, Argentina".
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or less. Alpa Corral, El Talita and Los Cerros are the three largest individual plutons and together they make up the bulk of the batholith. The most common rock type is
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for the batholith are, contrary to other batholiths, largely undeformed. The relation of the magmatic episode represented by the Cerro Aspero Batholith to the
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occur in the batholith. At most veins reach 3 meters in thickness. Collectively these veins constitute the largest reserves of fluorite in the whole
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Coniglio, Jorge E.; D'eramo, Fernando J.; Pinotti, Lucio P.; Demartis, Manuel; Agulleiro Insúa, Leonardo A.; Petrelli, Hugo A. (2010).
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is not fully understood. Alternatively it is grouped as a "Achaliano" igneous cycle.
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covers an approximate area of 440 km and lies about 50 km south of the larger
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The emplacement of plutons occurred in the Middle to Late
207: 46:. The batholith contains various circular plutons 129: 127: 125: 123: 121: 227: 8: 171:Revista de la Asociación Geológica Argentina 234: 220: 138:Journal of South American Earth Sciences 117: 290:Geology of Córdoba Province, Argentina 16:Group of plutons in central Argentina 7: 188: 186: 96:Vertical to near-vertical veins of 206:. You can help Knowledge (XXG) by 74:but varies from coarse grained to 14: 190: 1: 310:Lithodemic units of Argentina 151:10.1016/S0895-9811(02)00033-0 285:Batholiths of South America 336: 185: 38:in central Argentina. The 28:batolito de Cerro Aspero 27: 20:Cerro Aspero Batholith 261:32.66667°S 64.00000°W 300:Geology of Argentina 266:-32.66667; -64.00000 257: /  305:Devonian magmatism 295:Devonian Argentina 91:Famatinian orogeny 54:at pressures of 2 315:Sierras Pampeanas 215: 214: 106:Sierras Pampeanas 36:Sierras Pampeanas 327: 272: 271: 269: 268: 267: 262: 258: 255: 254: 253: 250: 236: 229: 222: 194: 187: 180: 179: 161: 155: 154: 131: 87:Contact aureoles 44:Achala Batholith 30:) is a group of 335: 334: 330: 329: 328: 326: 325: 324: 275: 274: 265: 263: 259: 256: 251: 248: 246: 244: 243: 241: 240: 184: 183: 163: 162: 158: 133: 132: 119: 114: 66:and an igneous 17: 12: 11: 5: 333: 331: 323: 322: 317: 312: 307: 302: 297: 292: 287: 277: 276: 239: 238: 231: 224: 216: 213: 212: 195: 182: 181: 174:(in Spanish). 156: 145:(2): 251–265. 116: 115: 113: 110: 100:formed in the 15: 13: 10: 9: 6: 4: 3: 2: 332: 321: 320:Geology stubs 318: 316: 313: 311: 308: 306: 303: 301: 298: 296: 293: 291: 288: 286: 283: 282: 280: 273: 270: 237: 232: 230: 225: 223: 218: 217: 211: 209: 205: 202:article is a 201: 196: 193: 189: 177: 173: 172: 167: 160: 157: 152: 148: 144: 140: 139: 130: 128: 126: 124: 122: 118: 111: 109: 107: 103: 99: 94: 92: 88: 84: 79: 77: 73: 69: 65: 61: 57: 53: 49: 45: 41: 37: 33: 29: 25: 21: 242: 208:expanding it 197: 175: 169: 159: 142: 136: 95: 80: 72:equigranular 60:monzogranite 34:in southern 19: 18: 264: / 76:porphyritic 279:Categories 252:64°00′00″W 249:32°40′00″S 112:References 102:Cretaceous 40:batholith 98:fluorite 85:period. 83:Devonian 70:that is 48:emplaced 200:geology 68:texture 64:biotite 52:stoping 32:plutons 24:Spanish 108:area. 198:This 62:with 204:stub 178:(4). 56:kbar 147:doi 78:. 50:by 281:: 176:67 168:. 143:15 141:. 120:^ 26:: 235:e 228:t 221:v 210:. 153:. 149:: 22:(

Index

Spanish
plutons
Sierras Pampeanas
batholith
Achala Batholith
emplaced
stoping
kbar
monzogranite
biotite
texture
equigranular
porphyritic
Devonian
Contact aureoles
Famatinian orogeny
fluorite
Cretaceous
Sierras Pampeanas





Journal of South American Earth Sciences
doi
10.1016/S0895-9811(02)00033-0
"Control estructural de las mineralizaciones de fluorita del batolito Cerro Áspero, Sierras Pampeanas de Córdoba"
Revista de la Asociación Geológica Argentina
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