625:
477:
438:
2608:
2460:
450:
672:
296:
properties. Similarly, the range of chemical composition allows chlorite group minerals to exist over a wide range of temperature and pressure conditions. For this reason chlorite minerals are ubiquitous minerals within low and medium temperature metamorphic rocks, some igneous rocks,
47:
1011:
Clinochlore, pennantite, and chamosite are the most common varieties. Several other sub-varieties have been described. A massive compact variety of clinochlore used as a decorative carving stone is referred to by the trade name
1036:
Chlorite does not have any specific industrial uses of any importance. Some rock types containing chlorite, such as chlorite schist, have minor decorative uses or as construction stone. However, chlorite is a common mineral in
1044:
Chlorite schist has been used as roofing granules, the mineral granules adhered to asphalt composition shingles due to the green color. It was quarried near Ely, Minnesota, US, until superseded by synthetic materials.
1237:
Osacky, Marek; Geramian, Mirjavad; Ivey, Douglas G.; Liu, Qi; Etsell, Thomas H. (16 July 2015). "Influence of
Nonswelling Clay Minerals (Illite, Kaolinite, and Chlorite) on Nonaqueous Solvent Extraction of Bitumen".
579:
facies. This facies is characterized by temperatures near 450 °C (840 °F) and pressures near 5 kbar. At higher temperatures, much of the chlorite is destroyed by reactions with either
492:
Chlorite is a common mineral, found in metamorphic, igneous, and sedimentary rocks. It is an important rock-forming mineral in low- to medium-grade metamorphic rock formed by metamorphism of
280:
Chlorite minerals show a wide variety of compositions, in which magnesium, iron, aluminium, and silicon substitute for each other in the crystal structure. A complete
292:. In addition, manganese, zinc, lithium, and calcium species are known. The great range in composition results in considerable variation in physical, optical, and
1413:
Wilkinson, Jamie J.; Chang, Zhaoshan; Cooke, David R.; Baker, Michael J.; Wilkinson, Clara C.; Inglis, Shaun; Chen, Huayong; Bruce
Gemmell, J. (May 2015).
437:
431:
layers, but these are bonded together by individual cations (such as potassium, sodium, or calcium ions) rather than a positively charged brucite layer.
1636:
449:
2498:
520:
on the ocean floor is often altered to pure chlorite, in part by exchange of chemicals with seawater. The green color of many igneous rocks,
1590:
1527:
1159:
575:
identified the chlorite zone as the zone of mildest metamorphism. In modern petrology, chlorite is the diagnostic mineral of the
1361:
1209:
1184:
178:
1629:
500:
rock. It is also common in igneous rocks, usually as a secondary mineral, formed by alteration of mafic minerals such as
2637:
2632:
415:
layers of chlorite contain some aluminium in place of silicon, which gives the layers an overall negative charge. These
2491:
464:. It is a nonswelling clay mineral, since water is not adsorbed in the interlayer spaces, and it has a relatively low
602:. At still higher temperatures, other reactions destroy the remaining chlorite, often with release of water vapor.
1464:
Manthilake, Geeth; Bolfan-Casanova, Nathalie; Novella, Davide; Mookherjee, Mainak; Andrault, Denis (6 May 2016).
572:
1761:
2642:
1622:
610:
465:
298:
1736:
331:. However, while the plates are flexible, they are not elastic like mica, and are less easily pulled apart.
108:
2484:
1751:
606:
168:
1963:
1896:
624:
1741:
1535:
1477:
1426:
1092:
2430:
2359:
2127:
1986:
1916:
2435:
2200:
2157:
2021:
1846:
1801:
1791:
1716:
1696:
408:
315:(χλωρός), meaning "green", in reference to its color. Chlorite minerals do not contain the element
201:
191:
2240:
2235:
2225:
2142:
1871:
1816:
2402:
2397:
2374:
2147:
2089:
2074:
2044:
1944:
1906:
1776:
1746:
1711:
1681:
1110:
580:
568:
263:
158:
2195:
2132:
2114:
1891:
1836:
1831:
1821:
1701:
1598:
1466:"Dehydration of chlorite explains anomalously high electrical conductivity in the mantle wedges"
1267:"Physico-Chemical Properties of Clay Minerals and Their Use as a Health Promoting Feed Additive"
2336:
2162:
1886:
1726:
476:
2172:
2152:
2079:
1911:
1841:
1806:
1661:
1503:
1357:
1298:
1205:
1180:
1155:
645:
293:
2137:
1766:
1543:
1539:
1493:
1485:
1444:
1434:
1288:
1278:
1247:
1100:
1054:
528:
is due to fine particles of chlorite disseminated throughout the rock. Chlorite is a common
259:
221:
211:
69:
2612:
2558:
2464:
2425:
2205:
62:
1481:
1430:
1096:
1881:
1866:
1645:
1498:
1465:
1293:
1266:
1021:
309:
281:
277:
or other low-silica volcanic rock, typically contains significant amounts of chlorite.
252:
118:
2626:
2440:
2412:
1901:
1114:
517:
266:
148:
1251:
613:, where it occurs in the "green rock" environment with epidote, actinolite, albite,
2573:
2507:
2420:
2263:
2258:
2059:
1968:
1954:
1934:
1781:
481:
461:
399:) is often referred to as a talc layer, since talc is composed entirely of stacked
1439:
1414:
2354:
2326:
2273:
2230:
2186:
2094:
2064:
2049:
2039:
2001:
1013:
649:
629:
576:
285:
270:
1547:
2568:
2533:
2382:
2298:
2283:
2210:
2069:
2054:
2034:
1996:
1876:
1861:
1851:
1796:
1771:
1721:
1706:
1676:
1134:
1059:
671:
657:
653:
641:
557:
529:
505:
407:
layers of talc are electrically neutral and are bound only by relatively weak
123:
1265:
Nadziakiewicza, Małgorzata; Kehoe, Sylvia; Micek, Piotr (23 September 2019).
2583:
2553:
2548:
2538:
2518:
2387:
2364:
2346:
2331:
2321:
2313:
2288:
2268:
2220:
2167:
2122:
2104:
2084:
2006:
1978:
1826:
1811:
740:
595:
365:. This formula emphasizes the structure of the group, which is described as
289:
127:
17:
1507:
1489:
1449:
1356:. Harlow, Essex, England: Longman Scientific & Technical. p. 121.
1302:
46:
1521:
Grove TL, Chatterjee N, Parman SW, et al. (2006). "The influence of H
2588:
2578:
2392:
2278:
2215:
2182:
1856:
1731:
1666:
1415:"The chlorite proximitor: A new tool for detecting porphyry ore deposits"
1128:
798:
614:
584:
549:
509:
316:
31:
1561:
1105:
1080:
2563:
2528:
2303:
2099:
2029:
2011:
1991:
1691:
1686:
1283:
1025:
618:
591:
561:
537:
536:
and in sedimentary rock containing clay minerals. Chlorite is found in
501:
497:
424:
255:
443:
Crystal structure of chlorite viewed along (looking along the layers)
284:
series exists between the two most common end members, magnesium-rich
2543:
2293:
1786:
1671:
633:
599:
553:
545:
541:
525:
513:
485:
274:
427:
layers. Mica is also composed of aluminium-rich, negatively charged
656:, and chlorite may even be present in the mantle volume from which
1614:
1017:
670:
660:
521:
493:
455:
Chlorite structure viewed along showing pseudohexagonal structure
2593:
2476:
1939:
1926:
1756:
1653:
1038:
587:
533:
332:
328:
2480:
1618:
1335:
1333:
1331:
1329:
2453:
Structural groups mainly; based on rruff.info/ima, modified
1130:
Chlorite Group: Mineral information, data and localities
605:
Chlorite is one of the most common minerals produced by
153:
Foliated masses, scaley aggregates, disseminated flakes.
1562:"Seraphinite: Mineral information, data and localities"
1154:. New York: Oxford University Press. pp. 251–260.
1316:
1314:
1312:
143:
Various shades of green; rarely yellow, red, or white.
640:
Experiments indicate that chlorite can be stable in
335:
is much softer and feels soapy between the fingers.
2411:
2373:
2345:
2312:
2249:
2181:
2113:
2020:
1977:
1953:
1925:
1652:
1200:Klein, Cornelis; Hurlbut, Cornelius S. Jr. (1993).
238:
230:
220:
210:
200:
190:
177:
167:
157:
147:
139:
134:
117:
107:
68:
58:
53:
39:
1202:Manual of mineralogy : (after James D. Dana)
419:layers are bound together by positively charged
1204:(21st ed.). New York: Wiley. p. 514.
1179:. Princeton, N.J.: Van Nostrand. p. 486.
327:Chlorite forms blue-green crystals resembling
2492:
1630:
480:Quartz crystal with chlorite inclusions from
8:
1339:
1224:
338:The typical general formula for chlorite is
1145:
1143:
2499:
2485:
2477:
1637:
1623:
1615:
1497:
1448:
1438:
1292:
1282:
1104:
1354:An introduction to metamorphic petrology
1000:
996:
992:
988:
984:
968:
964:
960:
956:
940:
936:
932:
928:
912:
908:
904:
900:
884:
880:
876:
872:
868:
852:
848:
844:
840:
836:
820:
816:
812:
808:
790:
786:
782:
778:
762:
758:
754:
750:
732:
728:
724:
720:
704:
700:
696:
692:
680:
636:from Michigan (size: 3.5 × 3.1 × 2.7 cm)
623:
475:
361:
357:
353:
349:
345:
341:
100:
96:
92:
88:
84:
80:
1400:
1388:
1376:
1071:
1016:. It occurs in the Korshunovskoye iron
433:
319:, also named from the same Greek root.
556:, and is also found in associate with
36:
1320:
7:
1081:"IMA–CNMNC approved mineral symbols"
1041:, which has a vast number of uses.
301:rocks and deeply buried sediments.
1419:Journal of Geochemical Exploration
25:
2606:
2458:
448:
436:
45:
1252:10.1021/acs.energyfuels.5b00269
1:
667:Members of the chlorite group
532:product and is widespread in
1525:O on mantle wedge melting".
1440:10.1016/j.gexplo.2015.01.005
369:and consists of alternating
273:, formed by metamorphism of
234:Folia flexible – not elastic
30:For the chemistry term, see
571:in the Scottish Highlands,
2659:
1762:Fluorotetraferriphlogopite
1548:10.1016/j.epsl.2006.06.043
1352:Yardley, B. W. D. (1989).
1152:Introduction to mineralogy
1150:Nesse, William D. (2000).
567:In his pioneering work on
488:(size: 4.2 × 3.9 × 3.3 cm)
29:
2602:
2514:
2449:
460:Chlorite is considered a
423:layers, sometimes called
44:
1528:Earth Planet. Sci. Lett.
1340:Klein & Hurlbut 1993
1225:Klein & Hurlbut 1993
1175:Sinkankas, John (1964).
466:cation exchange capacity
1540:2006E&PSL.249...74G
1177:Mineralogy for amateurs
1737:Ferroaluminoceladonite
1490:10.1126/sciadv.1501631
1085:Mineralogical Magazine
676:
637:
489:
196:Vitreous, pearly, dull
674:
627:
607:propylitic alteration
516:. The glassy rims of
479:
231:Other characteristics
611:hydrothermal systems
409:van der Waals forces
258:common in low-grade
2638:Monoclinic minerals
2633:Clay minerals group
2613:Minerals portal
2465:Minerals portal
1752:Fluorokinoshitalite
1601:on 12 November 2004
1482:2016SciA....2E1631M
1431:2015JCExp.152...10W
1227:, pp. 500–501.
1106:10.1180/mgm.2021.43
1097:2021MinM...85..291W
1079:Warr, L.N. (2021).
411:. By contrast, the
1284:10.3390/ani9100714
1240:Energy & Fuels
951:chlinochlore var.
677:
638:
581:potassium feldspar
569:metamorphic facies
490:
206:Pale green to grey
2620:
2619:
2474:
2473:
1964:Ferripyrophyllite
1807:Manganiceladonite
1662:Aluminoceladonite
1403:, pp. 64–68.
1007:
1006:
260:metamorphic rocks
251:are the group of
245:
244:
16:(Redirected from
2650:
2611:
2610:
2609:
2501:
2494:
2487:
2478:
2463:
2462:
2461:
1897:Tetraferriannite
1757:Fluorophlogopite
1639:
1632:
1625:
1616:
1610:
1608:
1606:
1597:. Archived from
1577:
1576:
1574:
1572:
1558:
1552:
1551:
1518:
1512:
1511:
1501:
1470:Science Advances
1461:
1455:
1454:
1452:
1442:
1410:
1404:
1398:
1392:
1386:
1380:
1374:
1368:
1367:
1349:
1343:
1337:
1324:
1318:
1307:
1306:
1296:
1286:
1262:
1256:
1255:
1246:(7): 4150–4159.
1234:
1228:
1222:
1216:
1215:
1197:
1191:
1190:
1172:
1166:
1165:
1147:
1138:
1137:
1125:
1119:
1118:
1108:
1076:
1055:List of minerals
1003:
971:
943:
915:
887:
855:
823:
793:
765:
735:
707:
681:
652:carried down by
648:above the ocean
452:
440:
364:
222:Refractive index
212:Specific gravity
183:
103:
75:
74:(repeating unit)
49:
37:
21:
2658:
2657:
2653:
2652:
2651:
2649:
2648:
2647:
2643:Phyllosilicates
2623:
2622:
2621:
2616:
2607:
2605:
2598:
2559:Montmorillonite
2510:
2505:
2475:
2470:
2459:
2457:
2445:
2426:Franklinphilite
2407:
2369:
2341:
2308:
2245:
2206:Montmorillonite
2177:
2109:
2016:
1973:
1949:
1921:
1742:Ferroceladonite
1648:
1646:Phyllosilicates
1643:
1604:
1602:
1589:
1586:
1584:Further reading
1581:
1580:
1570:
1568:
1560:
1559:
1555:
1524:
1520:
1519:
1515:
1476:(5): e1501631.
1463:
1462:
1458:
1412:
1411:
1407:
1399:
1395:
1387:
1383:
1375:
1371:
1364:
1351:
1350:
1346:
1338:
1327:
1319:
1310:
1264:
1263:
1259:
1236:
1235:
1231:
1223:
1219:
1212:
1199:
1198:
1194:
1187:
1174:
1173:
1169:
1162:
1149:
1148:
1141:
1127:
1126:
1122:
1078:
1077:
1073:
1068:
1051:
1034:
1020:deposit in the
1002:
998:
994:
990:
986:
982:
970:
966:
962:
958:
954:
942:
938:
934:
930:
926:
914:
910:
906:
902:
898:
886:
882:
878:
874:
870:
866:
854:
850:
846:
842:
838:
834:
822:
818:
814:
810:
806:
792:
788:
784:
780:
776:
764:
760:
756:
752:
748:
734:
730:
726:
722:
718:
706:
702:
698:
694:
690:
675:Chlorite schist
669:
663:are generated.
474:
456:
453:
444:
441:
363:
359:
355:
351:
347:
343:
339:
325:
181:
126:2/m; with some
102:
98:
94:
90:
86:
82:
78:
73:
72:
63:Phyllosilicates
35:
28:
27:Type of mineral
23:
22:
15:
12:
11:
5:
2656:
2654:
2646:
2645:
2640:
2635:
2625:
2624:
2618:
2617:
2603:
2600:
2599:
2597:
2596:
2591:
2586:
2581:
2576:
2571:
2566:
2561:
2556:
2551:
2546:
2541:
2536:
2531:
2526:
2521:
2515:
2512:
2511:
2506:
2504:
2503:
2496:
2489:
2481:
2472:
2471:
2469:
2468:
2454:
2450:
2447:
2446:
2444:
2443:
2438:
2433:
2431:Lennilenapeite
2428:
2423:
2417:
2415:
2413:Stilpnomelanes
2409:
2408:
2406:
2405:
2400:
2395:
2390:
2385:
2379:
2377:
2371:
2370:
2368:
2367:
2362:
2360:Ferrisepiolite
2357:
2351:
2349:
2343:
2342:
2340:
2339:
2334:
2329:
2324:
2318:
2316:
2310:
2309:
2307:
2306:
2301:
2296:
2291:
2286:
2281:
2276:
2271:
2266:
2261:
2255:
2253:
2247:
2246:
2244:
2243:
2238:
2233:
2228:
2223:
2218:
2213:
2208:
2203:
2198:
2192:
2190:
2179:
2178:
2176:
2175:
2170:
2165:
2160:
2155:
2150:
2145:
2140:
2135:
2130:
2128:Brinrobertsite
2125:
2119:
2117:
2111:
2110:
2108:
2107:
2102:
2097:
2092:
2087:
2082:
2077:
2072:
2067:
2062:
2057:
2052:
2047:
2042:
2037:
2032:
2026:
2024:
2018:
2017:
2015:
2014:
2009:
2004:
1999:
1994:
1989:
1987:Bismutoferrite
1983:
1981:
1975:
1974:
1972:
1971:
1966:
1960:
1958:
1951:
1950:
1948:
1947:
1942:
1937:
1931:
1929:
1923:
1922:
1920:
1919:
1917:Yangzhumingite
1914:
1909:
1904:
1899:
1894:
1889:
1884:
1882:Siderophyllite
1879:
1874:
1869:
1867:Polylithionite
1864:
1859:
1854:
1849:
1844:
1839:
1834:
1829:
1824:
1819:
1814:
1809:
1804:
1799:
1794:
1789:
1784:
1779:
1774:
1769:
1764:
1759:
1754:
1749:
1744:
1739:
1734:
1729:
1724:
1719:
1714:
1709:
1704:
1699:
1694:
1689:
1684:
1679:
1674:
1669:
1664:
1658:
1656:
1650:
1649:
1644:
1642:
1641:
1634:
1627:
1619:
1613:
1612:
1585:
1582:
1579:
1578:
1566:www.mindat.org
1553:
1534:(1–2): 74–89.
1522:
1513:
1456:
1405:
1393:
1381:
1369:
1362:
1344:
1342:, p. 522.
1325:
1323:, p. 252.
1308:
1257:
1229:
1217:
1210:
1192:
1185:
1167:
1160:
1139:
1120:
1091:(3): 291–320.
1070:
1069:
1067:
1064:
1063:
1062:
1057:
1050:
1047:
1033:
1030:
1022:Irkutsk Oblast
1009:
1008:
1005:
1004:
980:
977:
973:
972:
952:
949:
945:
944:
924:
921:
917:
916:
896:
893:
889:
888:
864:
861:
857:
856:
832:
829:
825:
824:
804:
801:
795:
794:
774:
771:
767:
766:
746:
743:
737:
736:
716:
713:
709:
708:
688:
685:
668:
665:
646:Earth's mantle
590:which produce
473:
470:
458:
457:
454:
447:
445:
442:
435:
324:
321:
288:and iron-rich
282:solid solution
253:phyllosilicate
243:
242:
240:
236:
235:
232:
228:
227:
224:
218:
217:
214:
208:
207:
204:
198:
197:
194:
188:
187:
184:
175:
174:
171:
165:
164:
161:
155:
154:
151:
145:
144:
141:
137:
136:
135:Identification
132:
131:
121:
119:Crystal system
115:
114:
111:
105:
104:
76:
66:
65:
60:
56:
55:
51:
50:
42:
41:
40:Chlorite group
26:
24:
14:
13:
10:
9:
6:
4:
3:
2:
2655:
2644:
2641:
2639:
2636:
2634:
2631:
2630:
2628:
2615:
2614:
2601:
2595:
2592:
2590:
2587:
2585:
2582:
2580:
2577:
2575:
2572:
2570:
2567:
2565:
2562:
2560:
2557:
2555:
2552:
2550:
2547:
2545:
2542:
2540:
2537:
2535:
2532:
2530:
2527:
2525:
2522:
2520:
2517:
2516:
2513:
2509:
2508:Clay minerals
2502:
2497:
2495:
2490:
2488:
2483:
2482:
2479:
2467:
2466:
2455:
2452:
2451:
2448:
2442:
2441:Stilpnomelane
2439:
2437:
2436:Parsettensite
2434:
2432:
2429:
2427:
2424:
2422:
2419:
2418:
2416:
2414:
2410:
2404:
2401:
2399:
2396:
2394:
2391:
2389:
2386:
2384:
2381:
2380:
2378:
2376:
2372:
2366:
2363:
2361:
2358:
2356:
2353:
2352:
2350:
2348:
2344:
2338:
2335:
2333:
2330:
2328:
2325:
2323:
2320:
2319:
2317:
2315:
2311:
2305:
2302:
2300:
2297:
2295:
2292:
2290:
2287:
2285:
2282:
2280:
2277:
2275:
2272:
2270:
2267:
2265:
2262:
2260:
2257:
2256:
2254:
2252:
2248:
2242:
2239:
2237:
2234:
2232:
2229:
2227:
2224:
2222:
2219:
2217:
2214:
2212:
2209:
2207:
2204:
2202:
2201:Ferrosaponite
2199:
2197:
2194:
2193:
2191:
2188:
2184:
2180:
2174:
2171:
2169:
2166:
2164:
2161:
2159:
2158:Lunijianlaite
2156:
2154:
2151:
2149:
2146:
2144:
2141:
2139:
2136:
2134:
2131:
2129:
2126:
2124:
2121:
2120:
2118:
2116:
2112:
2106:
2103:
2101:
2098:
2096:
2093:
2091:
2088:
2086:
2083:
2081:
2078:
2076:
2073:
2071:
2068:
2066:
2063:
2061:
2058:
2056:
2053:
2051:
2048:
2046:
2043:
2041:
2038:
2036:
2033:
2031:
2028:
2027:
2025:
2023:
2019:
2013:
2010:
2008:
2005:
2003:
2000:
1998:
1995:
1993:
1990:
1988:
1985:
1984:
1982:
1980:
1976:
1970:
1967:
1965:
1962:
1961:
1959:
1956:
1952:
1946:
1943:
1941:
1938:
1936:
1933:
1932:
1930:
1928:
1924:
1918:
1915:
1913:
1910:
1908:
1905:
1903:
1902:Trilithionite
1900:
1898:
1895:
1893:
1890:
1888:
1885:
1883:
1880:
1878:
1875:
1873:
1870:
1868:
1865:
1863:
1860:
1858:
1855:
1853:
1850:
1848:
1847:Oxyphlogopite
1845:
1843:
1840:
1838:
1835:
1833:
1830:
1828:
1825:
1823:
1820:
1818:
1815:
1813:
1810:
1808:
1805:
1803:
1802:Luanshiweiite
1800:
1798:
1795:
1793:
1792:Kinoshitalite
1790:
1788:
1785:
1783:
1780:
1778:
1775:
1773:
1770:
1768:
1765:
1763:
1760:
1758:
1755:
1753:
1750:
1748:
1745:
1743:
1740:
1738:
1735:
1733:
1730:
1728:
1725:
1723:
1720:
1718:
1717:Chromphyllite
1715:
1713:
1710:
1708:
1705:
1703:
1700:
1698:
1697:Boromuscovite
1695:
1693:
1690:
1688:
1685:
1683:
1680:
1678:
1675:
1673:
1670:
1668:
1665:
1663:
1660:
1659:
1657:
1655:
1651:
1647:
1640:
1635:
1633:
1628:
1626:
1621:
1620:
1617:
1600:
1596:
1592:
1588:
1587:
1583:
1567:
1563:
1557:
1554:
1549:
1545:
1541:
1537:
1533:
1530:
1529:
1517:
1514:
1509:
1505:
1500:
1495:
1491:
1487:
1483:
1479:
1475:
1471:
1467:
1460:
1457:
1451:
1450:10044/1/19967
1446:
1441:
1436:
1432:
1428:
1424:
1420:
1416:
1409:
1406:
1402:
1397:
1394:
1391:, p. 50.
1390:
1385:
1382:
1378:
1373:
1370:
1365:
1359:
1355:
1348:
1345:
1341:
1336:
1334:
1332:
1330:
1326:
1322:
1317:
1315:
1313:
1309:
1304:
1300:
1295:
1290:
1285:
1280:
1276:
1272:
1268:
1261:
1258:
1253:
1249:
1245:
1241:
1233:
1230:
1226:
1221:
1218:
1213:
1207:
1203:
1196:
1193:
1188:
1182:
1178:
1171:
1168:
1163:
1161:9780195106916
1157:
1153:
1146:
1144:
1140:
1136:
1132:
1131:
1124:
1121:
1116:
1112:
1107:
1102:
1098:
1094:
1090:
1086:
1082:
1075:
1072:
1065:
1061:
1058:
1056:
1053:
1052:
1048:
1046:
1042:
1040:
1031:
1029:
1027:
1023:
1019:
1015:
981:
978:
975:
974:
953:
950:
947:
946:
925:
922:
919:
918:
897:
894:
891:
890:
865:
862:
859:
858:
833:
830:
827:
826:
805:
802:
800:
797:
796:
775:
772:
769:
768:
747:
744:
742:
739:
738:
717:
714:
712:Borocookeite
711:
710:
691:(Zn,Fe,Al,Mg)
689:
686:
684:Baileychlore
683:
682:
679:
678:
673:
666:
664:
662:
659:
655:
651:
647:
643:
635:
631:
626:
622:
620:
616:
612:
608:
603:
601:
597:
593:
589:
586:
582:
578:
574:
570:
565:
563:
559:
555:
551:
547:
543:
539:
535:
531:
527:
523:
519:
518:pillow basalt
515:
511:
507:
503:
499:
495:
487:
483:
478:
471:
469:
467:
463:
451:
446:
439:
434:
432:
430:
426:
422:
418:
414:
410:
406:
402:
398:
397:
393:etrahedral =
392:
388:
384:
380:
376:
372:
368:
356:·(Mg,Fe)
336:
334:
330:
322:
320:
318:
314:
311:
307:
302:
300:
295:
291:
287:
283:
278:
276:
272:
268:
267:igneous rocks
265:
261:
257:
254:
250:
241:
237:
233:
229:
225:
223:
219:
215:
213:
209:
205:
203:
199:
195:
193:
189:
185:
180:
176:
172:
170:
166:
162:
160:
156:
152:
150:
149:Crystal habit
146:
142:
138:
133:
129:
125:
122:
120:
116:
112:
110:
106:
95:·(Mg,Fe)
77:
71:
67:
64:
61:
57:
52:
48:
43:
38:
33:
19:
2604:
2574:Palygorskite
2523:
2456:
2421:Bannisterite
2375:Pyrosmalites
2264:Borocookeite
2259:Baileychlore
2250:
2241:Yakhontovite
2236:Volkonskoite
2226:Swinefordite
2143:Hydrobiotite
2060:Cronstedtite
1969:Pyrophyllite
1955:Pyrophyllite
1935:Minnesotaite
1872:Preiswerkite
1817:Masutomilite
1782:Hendricksite
1603:. Retrieved
1599:the original
1595:Maricopa.edu
1594:
1569:. Retrieved
1565:
1556:
1531:
1526:
1516:
1473:
1469:
1459:
1422:
1418:
1408:
1401:Yardley 1989
1396:
1389:Yardley 1989
1384:
1379:, p. 8.
1377:Yardley 1989
1372:
1353:
1347:
1274:
1270:
1260:
1243:
1239:
1232:
1220:
1201:
1195:
1176:
1170:
1151:
1129:
1123:
1088:
1084:
1074:
1043:
1035:
1010:
979:IMA1966-027
770:Clinochlore
715:IMA2000-013
687:IMA1986-056
639:
604:
566:
491:
482:Minas Gerais
462:clay mineral
459:
428:
420:
416:
412:
404:
403:layers. The
400:
395:
394:
390:
386:
382:
378:
377:layers. The
374:
370:
366:
337:
326:
312:
308:is from the
305:
303:
299:hydrothermal
279:
248:
246:
18:Borocookeite
2403:Schallerite
2398:Pyrosmalite
2355:Falcondoite
2327:Chrysocolla
2274:Clinochlore
2231:Vermiculite
2187:vermiculite
2148:Karpinskite
2115:Corrensites
2090:Manandonite
2075:Guidottiite
2065:Fraipontite
2050:Caryopilite
2045:Brindleyite
2040:Berthierine
2022:Serpentines
2002:Hisingerite
1945:Willemseite
1907:Voloshinite
1777:Gorbunovite
1747:Fluorannite
1712:Chernykhite
1682:Balestraite
1277:(10): 714.
1024:of Eastern
1014:seraphinite
948:Ripidolite
923:year: 1946
920:Pennantite
895:year: 1968
863:year: 1955
831:year: 1940
828:Donbassite
803:year: 1866
773:year: 1851
745:year: 1820
650:lithosphere
630:pseudomorph
577:greenschist
573:G.M. Barrow
540:along with
385:etrahedral-
373:layers and
286:clinochlore
271:Greenschist
163:Perfect 001
130:polymorphs.
2627:Categories
2569:Nontronite
2534:Halloysite
2383:Friedelite
2347:Sepiolites
2314:Allophanes
2299:Pennantite
2284:Donbassite
2211:Nontronite
2196:Beidellite
2133:Corrensite
2070:Greenalite
2055:Chrysotile
2035:Antigorite
1997:Halloysite
1979:Kaolinites
1892:Tainiolite
1877:Roscoelite
1862:Phlogopite
1852:Paragonite
1837:Norrishite
1832:Nanpingite
1822:Montdorite
1797:Lepidolite
1772:Glauconite
1722:Clintonite
1707:Celadonite
1702:Bramallite
1677:Aspidolite
1591:"Chlorite"
1363:0582300967
1321:Nesse 2000
1211:047157452X
1186:0442276249
1135:Mindat.org
1066:References
1060:Thuringite
955:(Mg,Fe,Al)
899:(Ni,Mg,Al)
860:Gonyerite
658:island arc
654:subduction
642:peridotite
558:actinolite
530:weathering
506:hornblende
472:Occurrence
389:ctahedral-
323:Properties
239:References
179:Mohs scale
124:Monoclinic
109:IMA symbol
2584:Sepiolite
2554:Kaolinite
2549:Imogolite
2539:Hectorite
2519:Allophane
2388:Mcgillite
2365:Sepiolite
2337:Neotocite
2332:Imogolite
2322:Allophane
2289:Gonyerite
2269:Chamosite
2251:Chlorites
2221:Sauconite
2183:Smectites
2168:Saliotite
2163:Rectorite
2123:Aliettite
2105:Pecoraite
2085:Lizardite
2007:Kaolinite
1887:Suhailite
1827:Muscovite
1812:Margarite
1727:Eastonite
1425:: 10–26.
1115:235729616
741:Chamosite
628:Chlorite
596:muscovite
304:The name
290:chamosite
249:chlorites
226:1.57–1.67
128:triclinic
2589:Smectite
2579:Saponite
2524:Chlorite
2393:Nelenite
2279:Cookeite
2216:Saponite
2173:Tosudite
2153:Kulkeite
2095:Népouite
2080:Kellyite
1912:Wonesite
1857:Phengite
1842:Orlovite
1732:Ephesite
1667:Anandite
1508:27386526
1303:31548509
1049:See also
976:Sudoite
843:][Si
799:Cookeite
615:hematite
585:phengite
550:sericite
510:pyroxene
317:chlorine
306:chlorite
256:minerals
182:hardness
173:Lamellar
169:Fracture
159:Cleavage
59:Category
32:chlorite
2564:Nacrite
2529:Dickite
2304:Sudoite
2138:Dozyite
2100:Odinite
2030:Amesite
2012:Nacrite
1992:Dickite
1767:Garmite
1692:Biotite
1687:Bityite
1536:Bibcode
1499:4928900
1478:Bibcode
1427:Bibcode
1294:6827059
1271:Animals
1093:Bibcode
1026:Siberia
987:(Al,Fe)
959:(Al,Si)
903:(Si,Al)
892:Nimite
867:(Mn,Mg)
839:[Al
777:(Mg,Fe)
749:(Fe,Mg)
695:(Al,Si)
644:of the
619:calcite
592:biotite
562:epidote
538:pelites
526:schists
502:biotite
498:pelitic
425:brucite
381:layer (
344:(Si,Al)
340:(Mg,Fe)
313:chloros
264:altered
262:and in
216:2.6–3.3
83:(Si,Al)
79:(Mg,Fe)
70:Formula
54:General
2544:Illite
2294:Nimite
2189:family
1957:series
1787:Illite
1672:Annite
1605:22 Mar
1571:22 Mar
1506:
1496:
1360:
1301:
1291:
1208:
1183:
1158:
1113:
931:Al)(Si
703:(O,OH)
661:magmas
634:garnet
632:after
617:, and
600:quartz
598:, and
554:garnet
552:, and
546:albite
542:quartz
524:, and
522:slates
514:garnet
486:Brazil
275:basalt
202:Streak
192:Luster
1927:Talcs
1654:Micas
1111:S2CID
1018:skarn
851:](OH)
781:Al(Si
753:Al(Si
512:, or
494:mafic
396:T-O-T
367:TOT-O
310:Greek
294:X-ray
186:2–2.5
140:Color
2594:Talc
2185:and
1940:Talc
1607:2019
1573:2019
1504:PMID
1358:ISBN
1299:PMID
1206:ISBN
1181:ISBN
1156:ISBN
1039:clay
1032:Uses
999:(OH)
967:(OH)
939:(OH)
935:Al)O
911:(OH)
883:(OH)
871:(Fe)
841:2.33
819:(OH)
815:Al)O
807:LiAl
789:(OH)
785:Al)O
761:(OH)
757:Al)O
731:(OH)
719:LiAl
588:mica
560:and
534:clay
360:(OH)
352:(OH)
333:Talc
329:mica
247:The
99:(OH)
91:(OH)
1544:doi
1532:249
1494:PMC
1486:doi
1445:hdl
1435:doi
1423:152
1289:PMC
1279:doi
1248:doi
1101:doi
995:AlO
927:(Mn
847:AlO
811:(Si
727:B)O
723:(Si
609:by
583:or
564:.
496:or
429:TOT
417:TOT
413:TOT
405:TOT
401:TOT
379:TOT
371:TOT
113:Chl
2629::
1593:.
1564:.
1542:.
1502:.
1492:.
1484:.
1472:.
1468:.
1443:.
1433:.
1421:.
1417:.
1328:^
1311:^
1297:.
1287:.
1273:.
1269:.
1244:29
1242:.
1142:^
1133:,
1109:.
1099:.
1089:85
1087:.
1083:.
1028:.
997:10
991:Si
983:Mg
965:10
937:10
909:10
881:10
875:Si
849:10
835:Al
817:10
787:10
759:10
729:10
701:10
621:.
594:,
548:,
544:,
508:,
504:,
484:,
468:.
350:10
269:.
89:10
2500:e
2493:t
2486:v
1638:e
1631:t
1624:v
1611:]
1609:.
1575:.
1550:.
1546::
1538::
1523:2
1510:.
1488::
1480::
1474:2
1453:.
1447::
1437::
1429::
1366:.
1305:.
1281::
1275:9
1254:.
1250::
1214:.
1189:.
1164:.
1117:.
1103::
1095::
1001:8
993:3
989:3
985:2
969:8
963:O
961:4
957:6
941:8
933:3
929:5
913:8
907:O
905:4
901:6
885:8
879:O
877:3
873:2
869:5
853:8
845:3
837:2
821:8
813:3
809:4
791:8
783:3
779:5
763:8
755:3
751:5
733:8
725:3
721:4
705:8
699:O
697:4
693:6
421:O
391:T
387:O
383:T
375:O
362:6
358:3
354:2
348:O
346:4
342:3
101:6
97:3
93:2
87:O
85:4
81:3
34:.
20:)
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
