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Coesite

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rocks are carried to depths of 70 km (43 mi) or more. Coesite is formed at pressures above about 2.5 GPa (25 kbar) and temperature above about 700 °C. This corresponds to a depth of about 70 km in the Earth. It can be preserved as mineral inclusions in other phases because as it
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with each silicon atom surrounded by four oxygen atoms in a tetrahedron. Each oxygen atom is then bonded to two Si atoms to form a framework. There are two crystallographically distinct Si atoms and five different oxygen positions in the unit cell. Although the unit cell is close to being
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Korsakov, A.V.; Shatskiy, V. S. & Sobolev N.V. (1998). "Первая находка коэсита в эклогитах Кокчетавского массива (First occurrence of coesite in eclogites from the Kokchetav Massif)".
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is the most common host of such xenoliths. In metamorphic rocks, coesite is now recognized as one of the best mineral indicators of metamorphism at very high pressures (UHP, or
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Ghiribelli, B.; Frezzotti, M.L. & Palmeri, R. (2002). "Coesite in eclogites of the Lanterman Range (Antarctica): Evidence from textural and Raman studies".
1422: 1274:; Jay B Thomas; William O Nachlas; Paul G Fitzgerald (2020). "Evidence for ultrahigh-pressure metamorphism discovered in the Appalachian orogen". 1200:
O'Brien, P.J.; N. Zotov; R. Law; M.A. Khan; M.Q. Jan (2001). "Coesite in Himalayan eclogite and implications for models of India-Asia collision".
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Chopin, Christian (1984). "Coesite and pure pyrope in high-grade blueschists of the Western Alps: a first record and some consequences".
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within the stability field of quartz: coesite will eventually decay back into quartz with a consequent volume increase, although the
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Massonne, H.-J. (2001). "First find of coesite in the ultrahigh-pressure metamorphic area of the central Erzgebirge, Germany".
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is very slow at the low temperatures of the Earth's surface. The crystal symmetry is monoclinic C2/c, No.15,
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Smyth, Joseph R.; Hatton, C.J. (1977). "A coesite-sanidine grospydite from the Roberts Victor kimberlite".
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Smith, D.C. (1984). "Coesite in clinopyroxene in the Caledonides and its implications for geodynamics".
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Chao, E. C. T.; Shoemaker, E. M.; Madsen, B. M. (1960). "First Natural Occurrence of Coesite".
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Coesite has been identified in UHP metamorphic rocks around the world, including the western
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Anthony, John W.; Bideaux, Richard A.; Bladh, Kenneth W.; Nichols, Monte C., eds. (1995).
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and cannot be hexagonal. The crystal structure of coesite is similar to that of
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in shape ("a" and "c" are nearly equal and β nearly 120°), it is inherently
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explosion. It was not expected that coesite would survive in high pressure
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rings. The rings are further arranged into chains. This structure is
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Crossed-polars image of coesite grain (gray) ~1 mm across in
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Coes, Jr., L. (31 July 1953). "A New Dense Crystalline Silica".
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10.1130/0091-7613(2001)029<0435:CIHEAI>2.0.CO;2
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10.1130/0091-7613(1989)017<1085:CBEFTD>2.3.CO;2
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is pronounced as "Coze-ite", after chemist Loring Coes, Jr.
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In metamorphic rocks, coesite was initially described in
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In 1960, a natural occurrence of coesite was reported by
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of Germany, the Lanterman Range of Antarctica, in the
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Wang, Xiaomin; Liou, J. G.; Mao, H. K. (1989-12-01).
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in UHP metamorphic minerals up to 3 mm in size
2294: 981: 482:of the Earth that were carried up by ascending 1366:Barringer Meteor Crater science education page 413:) that is formed when very high pressure (2–3 1987: 1430: 1416: 934: 932: 618:, forming at higher pressure than stishovite 463: 1152: 1070: 900: 1994: 1980: 1423: 1409: 941:Contributions to Mineralogy and Petrology 929: 759: 669: 545: 16:Silica mineral, rare polymorph of quartz 2295: 938: 1975: 1404: 809: 494:). Such UHP metamorphic rocks record 644:"IMA–CNMNC approved mineral symbols" 641: 541: 2001: 1114:Schertl, H.-P.; Okay, A.I. (1994). 903:Earth and Planetary Science Letters 704:. Vol. 2 (Silica, Silicates). 498:or continental collisions in which 421:. Coesite was first synthesized by 13: 753: 14: 2334: 1354: 2272: 1523: 1517: 1387: 1373: 1317:Levien L.; Prewitt C.T. (1981). 1039:10.1127/0935-1221/2002/0014-0355 1004:10.1127/0935-1221/2001/0013-0565 710:Mineralogical Society of America 534:of Eastern Pakistan, and in the 368: 45:. Polycrystalline rim is quartz. 27: 1310: 1263: 1228: 1193: 1146: 1107: 1064: 1045: 1010: 492:ultrahigh-pressure metamorphism 1019:European Journal of Mineralogy 984:European Journal of Mineralogy 975: 894: 843: 803: 733: 686: 635: 432: 1: 1954:Lunar and Planetary Institute 1786:Cretaceous–Paleogene boundary 628: 624:, a higher-pressure polymorph 923:10.1016/0012-821X(77)90012-7 872:10.1126/science.132.3421.220 784:10.1126/science.118.3057.131 530:Range in Eastern China, the 514:of Italy at Dora Maira, the 7: 1846:Planar deformation features 609: 550:Atomic structure of coesite 10: 2339: 2318:Minerals in space group 15 1949:Impact Field Studies Group 821:Cambridge University Press 2268: 2225: 2202: 2154: 2147: 2126: 2098: 2065: 2012: 1884: 1753: 1532: 1515: 1456: 1438: 1432:Impact cratering on Earth 1332:: 324–333. Archived from 746:Dictionary.com Unabridged 354: 344: 334: 302: 294: 284: 274: 264: 254: 241: 229: 217: 204: 196: 186: 181: 151: 139: 121: 109: 99: 89: 70: 55: 50: 26: 21: 1919:William Kenneth Hartmann 1585:Clearwater East and West 1533:Confirmed≥20 km diameter 441:, in collaboration with 425:, Jr., a chemist at the 1836:Ordovician meteor event 915:1977E&PSL..34..284S 1939:Eugene Merle Shoemaker 1816:Late Heavy Bombardment 1054:Doklady Earth Sciences 702:Handbook of Mineralogy 649:Mineralogical Magazine 551: 526:region of Norway, the 522:of Kazakhstan, in the 468: 2303:Impact event minerals 1960:Traces of Catastrophe 1944:Earth Impact Database 1892:Ralph Belknap Baldwin 1326:American Mineralogist 571:and consists of four 549: 536:Appalachian Mountains 503:partially reverts to 467: 101:Strunz classification 1140:10.1127/ejm/6/6/0995 642:Warr, L. N. (2021). 600:metamorphic reaction 2313:Monoclinic minerals 2279:Minerals portal 1288:2020Geo....48..947G 1257:2019AGUFM.V51B..03G 1214:2001Geo....29..435O 1171:1989Geo....17.1085W 1132:1994EJMin...6..995S 1085:1984Natur.310..641S 1031:2002EJMin..14..355G 996:2001EJMin..13..565M 953:1984CoMP...86..107C 864:1960Sci...132..220C 776:1953Sci...118..131C 706:Chantilly, Virginia 671:10.1180/mgm.2021.43 662:2021MinM...85..291W 1856:Shock metamorphism 1761:Alvarez hypothesis 961:10.1007/BF00381838 816:The Diamond Makers 552: 469: 295:Optical properties 192:60.0843 g/mol 2308:Silica polymorphs 2290: 2289: 2286: 2285: 2174:Chrome chalcedony 2148:Notable varieties 2067:Cryptocrystalline 1969: 1968: 1909:Edward C. T. Chao 1270:Joseph Gonzalez; 1235:Joseph Gonzalez; 1165:(12): 1085–1088. 1079:(5979): 641–644. 830:978-0-521-65474-6 770:(3057): 131–132. 542:Crystal structure 459:metamorphic rocks 439:Edward C. T. Chao 361: 360: 290:2.92 (calculated) 135: 37:. Small, colored 2330: 2277: 2276: 2275: 2245:Herkimer diamond 2152: 2151: 1996: 1989: 1982: 1973: 1972: 1934:Peter H. Schultz 1897:Daniel Barringer 1806:Impact structure 1527: 1521: 1425: 1418: 1411: 1402: 1401: 1397: 1395:Chemistry portal 1392: 1391: 1390: 1383: 1378: 1377: 1348: 1347: 1345: 1344: 1338: 1323: 1314: 1308: 1307: 1296:10.1130/G47507.1 1267: 1261: 1260: 1245:AGU Fall Meeting 1232: 1226: 1225: 1197: 1191: 1190: 1150: 1144: 1143: 1111: 1105: 1104: 1093:10.1038/310641a0 1068: 1062: 1061: 1049: 1043: 1042: 1014: 1008: 1007: 979: 973: 972: 936: 927: 926: 898: 892: 891: 847: 841: 840: 838: 837: 813:(22 July 1999). 811:Hazen, Robert M. 807: 801: 795: 757: 751: 750: 737: 731: 730: 728: 726: 699: 690: 684: 683: 673: 639: 520:Kokchetav Massif 447:Barringer Crater 443:Eugene Shoemaker 394: 393: 390: 389: 386: 383: 380: 377: 374: 304:Refractive index 247: 129: 127:Prismatic (2/m) 85: 77: 76:(repeating unit) 31: 19: 18: 2338: 2337: 2333: 2332: 2331: 2329: 2328: 2327: 2323:Silicon dioxide 2293: 2292: 2291: 2282: 2273: 2271: 2264: 2221: 2198: 2143: 2122: 2094: 2061: 2008: 2000: 1970: 1965: 1914:Robert S. Dietz 1902:Barringer Medal 1880: 1791:Cryptoexplosion 1749: 1680:Puchezh-Katunki 1660:Nördlinger Ries 1528: 1522: 1513: 1479:Asia and Russia 1452: 1434: 1429: 1393: 1388: 1386: 1379: 1372: 1357: 1352: 1351: 1342: 1340: 1336: 1321: 1315: 1311: 1282:(10): 947–951. 1272:Suzanne Baldwin 1268: 1264: 1237:Suzanne Baldwin 1233: 1229: 1198: 1194: 1151: 1147: 1126:(6): 995–1000. 1120:Eur. J. Mineral 1112: 1108: 1069: 1065: 1050: 1046: 1015: 1011: 980: 976: 937: 930: 899: 895: 858:(3421): 220–2. 848: 844: 835: 833: 831: 808: 804: 758: 754: 739: 738: 734: 724: 722: 720: 697: 691: 687: 640: 636: 631: 612: 593: 589: 585: 581: 573:silicon dioxide 544: 435: 412: 401:silicon dioxide 371: 367: 329: 323: 321: 315: 313: 245: 173: 171: 166: 161: 128: 84: 80: 75: 74: 46: 17: 12: 11: 5: 2336: 2326: 2325: 2320: 2315: 2310: 2305: 2288: 2287: 2284: 2283: 2269: 2266: 2265: 2263: 2262: 2257: 2255:Shocked quartz 2252: 2247: 2242: 2237: 2231: 2229: 2223: 2222: 2220: 2219: 2214: 2208: 2206: 2200: 2199: 2197: 2196: 2191: 2186: 2181: 2176: 2171: 2166: 2160: 2158: 2149: 2145: 2144: 2142: 2141: 2136: 2130: 2128: 2124: 2123: 2121: 2120: 2115: 2113:Lechatelierite 2110: 2104: 2102: 2096: 2095: 2093: 2092: 2087: 2082: 2077: 2071: 2069: 2063: 2062: 2060: 2059: 2054: 2049: 2044: 2039: 2034: 2029: 2024: 2018: 2016: 2010: 2009: 1999: 1998: 1991: 1984: 1976: 1967: 1966: 1964: 1963: 1956: 1951: 1946: 1941: 1936: 1931: 1926: 1921: 1916: 1911: 1906: 1905: 1904: 1894: 1888: 1886: 1882: 1881: 1879: 1878: 1873: 1868: 1863: 1861:Shocked quartz 1858: 1853: 1848: 1843: 1838: 1833: 1828: 1823: 1821:Lechatelierite 1818: 1813: 1808: 1803: 1798: 1796:Ejecta blanket 1793: 1788: 1783: 1781:Complex crater 1778: 1773: 1768: 1763: 1757: 1755: 1751: 1750: 1748: 1747: 1742: 1737: 1732: 1727: 1722: 1717: 1712: 1707: 1702: 1697: 1692: 1687: 1682: 1677: 1672: 1667: 1662: 1657: 1652: 1647: 1642: 1637: 1632: 1627: 1622: 1617: 1612: 1607: 1602: 1597: 1592: 1587: 1582: 1577: 1575:Chesapeake Bay 1572: 1567: 1562: 1557: 1552: 1547: 1542: 1536: 1534: 1530: 1529: 1516: 1514: 1512: 1511: 1506: 1501: 1496: 1491: 1486: 1481: 1476: 1471: 1466: 1460: 1458: 1454: 1453: 1451: 1450: 1445: 1439: 1436: 1435: 1428: 1427: 1420: 1413: 1405: 1399: 1398: 1384: 1381:Science portal 1369: 1368: 1363: 1356: 1355:External links 1353: 1350: 1349: 1309: 1262: 1227: 1208:(5): 435–438. 1192: 1145: 1106: 1063: 1044: 1025:(2): 355–360. 1009: 990:(3): 565–570. 974: 947:(2): 107–118. 928: 893: 842: 829: 823:. p. 91. 802: 752: 749:(Online). n.d. 732: 718: 685: 656:(3): 291–320. 633: 632: 630: 627: 626: 625: 619: 611: 608: 604:Pearson symbol 591: 587: 583: 579: 578:arranged in Si 543: 540: 524:Western Gneiss 434: 431: 427:Norton Company 410: 359: 358: 356: 352: 351: 348: 342: 341: 338: 332: 331: 327: 319: 311: 306: 300: 299: 296: 292: 291: 288: 282: 281: 278: 272: 271: 268: 262: 261: 258: 252: 251: 248: 239: 238: 233: 227: 226: 221: 215: 214: 208: 202: 201: 198: 194: 193: 190: 184: 183: 182:Identification 179: 178: 155: 149: 148: 143: 137: 136: 125: 119: 118: 113: 111:Crystal system 107: 106: 103: 97: 96: 93: 87: 86: 82: 78: 68: 67: 57: 53: 52: 48: 47: 32: 24: 23: 15: 9: 6: 4: 3: 2: 2335: 2324: 2321: 2319: 2316: 2314: 2311: 2309: 2306: 2304: 2301: 2300: 2298: 2281: 2280: 2267: 2261: 2258: 2256: 2253: 2251: 2248: 2246: 2243: 2241: 2238: 2236: 2233: 2232: 2230: 2228: 2224: 2218: 2215: 2213: 2210: 2209: 2207: 2205: 2201: 2195: 2192: 2190: 2187: 2185: 2182: 2180: 2177: 2175: 2172: 2170: 2167: 2165: 2162: 2161: 2159: 2157: 2153: 2150: 2146: 2140: 2137: 2135: 2132: 2131: 2129: 2127:Miscellaneous 2125: 2119: 2116: 2114: 2111: 2109: 2106: 2105: 2103: 2101: 2097: 2091: 2088: 2086: 2083: 2081: 2078: 2076: 2073: 2072: 2070: 2068: 2064: 2058: 2055: 2053: 2050: 2048: 2045: 2043: 2040: 2038: 2035: 2033: 2030: 2028: 2025: 2023: 2020: 2019: 2017: 2015: 2011: 2007: 2004: 1997: 1992: 1990: 1985: 1983: 1978: 1977: 1974: 1962: 1961: 1957: 1955: 1952: 1950: 1947: 1945: 1942: 1940: 1937: 1935: 1932: 1930: 1927: 1925: 1924:H. Jay Melosh 1922: 1920: 1917: 1915: 1912: 1910: 1907: 1903: 1900: 1899: 1898: 1895: 1893: 1890: 1889: 1887: 1883: 1877: 1874: 1872: 1869: 1867: 1864: 1862: 1859: 1857: 1854: 1852: 1849: 1847: 1844: 1842: 1839: 1837: 1834: 1832: 1829: 1827: 1824: 1822: 1819: 1817: 1814: 1812: 1809: 1807: 1804: 1802: 1801:Impact crater 1799: 1797: 1794: 1792: 1789: 1787: 1784: 1782: 1779: 1777: 1774: 1772: 1769: 1767: 1764: 1762: 1759: 1758: 1756: 1752: 1746: 1743: 1741: 1738: 1736: 1733: 1731: 1728: 1726: 1723: 1721: 1718: 1716: 1713: 1711: 1708: 1706: 1705:Slate Islands 1703: 1701: 1698: 1696: 1693: 1691: 1688: 1686: 1683: 1681: 1678: 1676: 1673: 1671: 1668: 1666: 1663: 1661: 1658: 1656: 1653: 1651: 1648: 1646: 1643: 1641: 1638: 1636: 1633: 1631: 1628: 1626: 1623: 1621: 1618: 1616: 1613: 1611: 1608: 1606: 1603: 1601: 1598: 1596: 1593: 1591: 1588: 1586: 1583: 1581: 1578: 1576: 1573: 1571: 1568: 1566: 1563: 1561: 1558: 1556: 1553: 1551: 1548: 1546: 1543: 1541: 1538: 1537: 1535: 1531: 1526: 1520: 1510: 1507: 1505: 1502: 1500: 1499:South America 1497: 1495: 1494:North America 1492: 1490: 1487: 1485: 1482: 1480: 1477: 1475: 1472: 1470: 1467: 1465: 1462: 1461: 1459: 1455: 1449: 1446: 1444: 1443:Impact crater 1441: 1440: 1437: 1433: 1426: 1421: 1419: 1414: 1412: 1407: 1406: 1403: 1396: 1385: 1382: 1376: 1371: 1367: 1364: 1362: 1359: 1358: 1339:on 2016-06-04 1335: 1331: 1327: 1320: 1313: 1305: 1301: 1297: 1293: 1289: 1285: 1281: 1277: 1273: 1266: 1258: 1254: 1250: 1246: 1242: 1238: 1231: 1223: 1219: 1215: 1211: 1207: 1203: 1196: 1188: 1184: 1180: 1176: 1172: 1168: 1164: 1160: 1156: 1149: 1141: 1137: 1133: 1129: 1125: 1121: 1117: 1110: 1102: 1098: 1094: 1090: 1086: 1082: 1078: 1074: 1067: 1059: 1055: 1048: 1040: 1036: 1032: 1028: 1024: 1020: 1013: 1005: 1001: 997: 993: 989: 985: 978: 970: 966: 962: 958: 954: 950: 946: 942: 935: 933: 924: 920: 916: 912: 908: 904: 897: 889: 885: 881: 877: 873: 869: 865: 861: 857: 853: 846: 832: 826: 822: 818: 817: 812: 806: 799: 793: 789: 785: 781: 777: 773: 769: 765: 764: 756: 748: 747: 742: 736: 721: 715: 711: 707: 703: 696: 689: 681: 677: 672: 667: 663: 659: 655: 651: 650: 645: 638: 634: 623: 620: 617: 614: 613: 607: 605: 601: 597: 577: 574: 570: 566: 562: 557: 556:tectosilicate 554:Coesite is a 548: 539: 537: 533: 529: 525: 521: 517: 516:Ore Mountains 513: 508: 506: 501: 497: 493: 489: 485: 481: 477: 474: 466: 462: 460: 456: 452: 448: 444: 440: 430: 428: 424: 420: 416: 409: 406: 402: 398: 395:) is a form ( 392: 365: 357: 353: 349: 347: 343: 339: 337: 336:Birefringence 333: 326: 318: 310: 307: 305: 301: 297: 293: 289: 287: 283: 279: 277: 273: 269: 267: 263: 259: 257: 253: 249: 244: 240: 237: 234: 232: 228: 225: 222: 220: 216: 212: 209: 207: 206:Crystal habit 203: 199: 195: 191: 189: 185: 180: 176: 170:= 7.143  169: 164: 159: 156: 154: 150: 147: 144: 142: 138: 133: 126: 124: 123:Crystal class 120: 117: 114: 112: 108: 104: 102: 98: 94: 92: 88: 79: 73: 69: 65: 61: 60:Tectosilicate 58: 54: 49: 44: 40: 36: 30: 25: 20: 2270: 2250:Smoky quartz 2027:Cristobalite 2021: 1958: 1929:Graham Ryder 1851:Shatter cone 1841:Philippinite 1775: 1690:Saint Martin 1685:Rochechouart 1590:Gosses Bluff 1545:Amelia Creek 1448:Impact event 1361:Coesite page 1341:. 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Index


eclogite
inclusion
pyroxene
Tectosilicate
quartz
Formula
IMA symbol
Strunz classification
Crystal system
Monoclinic
Crystal class
H–M symbol
Space group
Unit cell
Formula mass
Crystal habit
Inclusions
Fracture
Conchoidal
Tenacity
Brittle
Mohs scale
Luster
Streak
Diaphaneity
Density
Refractive index
Birefringence
2V angle

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