2256:
2108:
29:
589:
The problem of mistaken identity arises when comparing dickite to other kaolin minerals due to the fact that kaolinite, dickite, and nacrite all have the same formula but different molecular structures. The only way to determine the true identity of the mineral is through powder x-ray diffraction and
787:
An experiment was conducted using a pseudo-hexagonal crystal of dickite to determine the unit cell information and the layers that exist within dickite. It was found that there are six layers within the kaolin layer within dickite. This is evidenced in the following findings. There is an oxygen atom
783:
The hexagonal network of Si-O tetrahedra along with the superimposed layer of Al-O, OH octahedra make up the kaolin layer found in dickite. Dickite is composed of regular sequences of one, two and six kaolin layers. Analysis of the dickite structure reveals the space group to be C4s-Cc. The a and c
755:
and its crystal class is domatic (m). This crystal system contains two non-equal axes (a and b) that are perpendicular to each other and a third axis (c) that is inclined with respect to the a axis. The a and c axes lie in a plane. Dickite involves an interlayer bonding with at least 3 identifiable
742:
The hexagonal structure and the stacking of the atoms influence the physical properties in many ways including the color, hardness, cleavage, density, and luster. Another important factor in influencing physical properties of minerals is the presence of bonding between atoms. Within dickite there
617:
are a suitable environment for dickite. Very low pressure and high temperatures are the ideal environment for the formation of dickite. The more perfected crystallization of dickite occurs in porous algal limestones in the form of a white powder. The more disordered dickites can be found in less
738:
The atomic structure of dickite, being very similar to that of kaolinite and other kaolin type minerals, has a very specific arrangement that differs slightly enough to set its physical appearance and other physical properties apart from that of its family members kaolinite and nacrite. In a
784:
axis both lie on the glide plane of symmetry. Dickite's structure is made up of a shared layer of corner-sharing tetrahedra filled by a plane of oxygens and hydroxyls along with a sheet of edge-sharing octahedra with every third site left empty.
799:
which are parallel to the a-b plane stacked on top of one another which they found to be exactly as Gruner had described. It was also concluded that the two dimensional arrangement of some of the atoms are not as Gruner described.
633:
set in a matrix of greenish dickite, to discrete veins and surface coatings of white, cream and translucent dickite. It appears that dickite in the northerly zone were formed by hot ascending waters from an uncertain origin.
606:, Wales, UK. Dickite is scattered across Wales forming occurrences in vein assemblages and as a rock-forming mineral. This area and others where dickite can be found all share similar characteristics. Pockets in phylloid
731:. This is attributed to its loose chemical bonds. It is held with hydrogen bonds, which are otherwise weak. It leaves a white streak and it has a pearly luster. It has a density of 2.6. Dickite is biaxial, its
739:
comparison of the family of minerals through experiments examined by Ross and Kerr the similarities between them are clearly evident and can, depending on the samples, be indistinguishable by optical means.
768:
between oxygen atoms on the surface of one layer and hydroxyl groups on the opposing surface. A hydrogen bond, as the term is used here, involves a long range interaction between hydrogen of a
735:
is between 0.0050–0.0090, its surface relief is low and it has no dispersion. The plane of the optical axis is normal to the plane of symmetry and inclined 160, rear to the normal to (0,0,1).
586:. Through its evolution, dickite, a phyllosilicate mineral, maintains the aluminium and silicon elements influencing the formation of hexagonal sheets common to clay minerals.
704:
which allowed the dickite to be deposited in this area and it might be conclusive to say that this trend follows elsewhere in other locations around the world.
1009:
504:. It was not until 1931 that Clarence S. Ross and Paul F. Kerr looked closer at the mineral and concluded that it was different from the known minerals of
788:
from the all oxygen layer that lies at the center. The atoms of the O layer, the Si layer and the O, (OH) layer are situated for the ideal kaolin layer.
1284:
2146:
776:
and an oxygen atom coordinated to another cation. The reaction is predominantly electrostatic; hence an ionic bonding model is appropriate. Its
421:
Dickite occurs with other clays and requires x-ray diffraction for its positive identification. Dickite is an important alteration indicator in
621:
Another occurrence spot, as indicated by
Brindley and Porter of the American Mineralogists journal, is the Northerly dickite-bearing zone in
964:
2300:
791:
X-ray experiments were performed by C. J. Ksanda and Tom F. W. Barth and it was concluded that dickite is composed of tiny layers of
881:
97:
712:
Dickite takes on the appearance of a white, brown earthy color and is often found embedded in many other minerals such as quartz.
715:
Dickite has perfect cleavage in the (001) direction. Its color varies from blue, gray, white to colorless. It usually has a dull
391:
1225:
Fialips CI, Majzlan J, Beaufort D, et al. (2003). "New thermochemical evidence on the stability of dickite vs. kaolinite".
538:
is the chemical formula of dickite. The calculated percent abundances are very close when compared to other kaolin minerals.
214:
448:, United Kingdom, where it was first described in 1888. Dickite appears in locations with similar qualities and is found in
1277:
247:
2295:
2290:
2285:
2139:
107:
752:
1409:
2280:
1270:
1384:
1041:"Genesis and Evolution of the Kaolin-group Minerals During the Diagenesis and the Beginning of Metamorphism"
666:
429:
87:
1094:
Schroeder RJ, Hayes JB (1968). "Dickite and
Kaolinite in Pennsylvanian Limestones of Southeastern Kansas".
2132:
1142:
972:
1399:
1227:
1201:
1073:
1014:
204:
1611:
1544:
1389:
1235:
1103:
829:
761:
359:
2078:
2007:
1775:
1634:
1564:
1199:
Brindley GW, Porter AR (1978). "Occurrence of dickite in
Jamaica-ordered and disordered varieties".
2083:
1848:
1805:
1669:
1494:
1449:
1439:
1364:
1344:
237:
227:
1888:
1883:
1873:
1790:
1519:
1464:
433:
2050:
2045:
2022:
1795:
1737:
1722:
1692:
1592:
1554:
1424:
1394:
1359:
1329:
1251:
1209:
980:
847:
701:
194:
1843:
1780:
1762:
1539:
1484:
1479:
1469:
1349:
676:
In the dickite deposits of southeast Kansas the distribution is dependent on the following: the
629:
containing cream to pinkish and purplish fragments composed largely of dickite with subordinate
1984:
1810:
1534:
1374:
1175:
Occurrence and microscopic examination of reference clay
Mineral specimens: Preliminary reports
1040:
1820:
1800:
1727:
1559:
1489:
1454:
1309:
1178:
887:
877:
689:
646:
348:
159:
1785:
1414:
1177:. American Petroleum Institute Research Project. Vol. 4. New York: Columbia University.
1243:
1150:
1111:
837:
654:
599:
441:
275:
257:
56:
49:
2260:
2206:
2112:
2073:
1853:
638:
44:
1239:
1107:
833:
2171:
1898:
1529:
1514:
1293:
1173:
Holmes RJ (1951). "Reference Clay
Localities". In Ker PF, Main MS, Hamilton PK (eds.).
769:
765:
697:
685:
465:
117:
2274:
2088:
2060:
1549:
851:
732:
677:
662:
469:
297:
184:
129:
1213:
2221:
2155:
2068:
1911:
1906:
1707:
1616:
1602:
1582:
1429:
1255:
501:
422:
351:
1065:
2002:
1974:
1921:
1878:
1834:
1742:
1712:
1697:
1687:
1649:
777:
693:
147:
500:
to conduct research on kaolin. He performed various experiments describing the
28:
2216:
2181:
2030:
1946:
1931:
1858:
1717:
1702:
1682:
1644:
1524:
1509:
1499:
1444:
1419:
1369:
1354:
1324:
1155:
1137:
1115:
757:
720:
493:
387:
355:
138:
122:
1182:
2231:
2201:
2196:
2186:
2166:
2035:
2012:
1994:
1979:
1969:
1961:
1936:
1916:
1868:
1815:
1770:
1752:
1732:
1654:
1626:
1474:
1459:
891:
614:
610:
583:
505:
415:
403:
379:
363:
935:
866:
1247:
578:
Dickite and other kaolin minerals are commonly developed by weathering of
2236:
2226:
2040:
1926:
1863:
1830:
1504:
1379:
1314:
700:
which made its way up-dip and through the intrusions in the conduit-like
650:
642:
603:
579:
497:
395:
371:
307:
842:
817:
2211:
1951:
1747:
1677:
1659:
1339:
1334:
910:
792:
665:. An extensive study was done on dickite pertaining to its location in
630:
626:
622:
509:
477:
461:
453:
407:
383:
367:
2191:
1941:
1434:
1319:
796:
773:
728:
670:
481:
457:
437:
411:
375:
189:
Pseudohexagonal crystals, aggregates of platelets and compact massive
1262:
681:
607:
473:
449:
445:
2241:
2124:
1587:
1574:
1404:
1301:
724:
716:
658:
512:. They named it after the first person to describe the mineral.
399:
2128:
1266:
760:
type interaction due to net unbalanced charges on the layers,
743:
exists dominant O-H bonding, a type of strong ionic bonding.
2101:
Structural groups mainly; based on rruff.info/ima, modified
1010:"Note on the Structure of Dickite and Other Clay Minerals"
661:, US, where the mineral is thought to be associated with
688:, thick deposits of highly porous algal limestones, and
358:
chemist Allan Brugh Dick, who first described it. It is
865:
Anthony JW, Bideaux RA, Bladh KW, et al. (1995).
2059:
2021:
1993:
1960:
1897:
1829:
1761:
1668:
1625:
1601:
1573:
1300:
911:"Dickite: Mineral information, data and localities"
316:
306:
296:
274:
266:
256:
246:
236:
226:
213:
203:
193:
183:
175:
170:
158:
146:
128:
116:
106:
96:
86:
55:
40:
35:
21:
492:In 1888, Allan Brugh Dick (1833–1926), a Scottish
425:systems as well as occurring in soils and shales.
394:). Dickite sometimes contains impurities such as
637:Dickite is found worldwide in locations such as
625:. The dickite in this zone ranges from indurate
2140:
1278:
8:
166:c = 14.424 ; β = 96.8°; Z = 4
2147:
2133:
2125:
1285:
1271:
1263:
876:. Tucson, Ariz.: Mineral Data Publishing.
390:, but with a different crystal structure (
27:
1194:
1192:
1154:
841:
649:, Mexico, in a silicified zone among the
1131:
1129:
1127:
1125:
1048:University of the Basque Country Seminar
905:
903:
901:
613:, in interstices of biocalcarenites and
569:
560:
556:
547:
534:
530:
526:
522:
343:
339:
335:
331:
79:
75:
71:
67:
1168:
1166:
1089:
1087:
1003:
1001:
808:
1059:
1057:
1034:
1032:
1030:
1028:
958:
956:
179:White, with coloration from impurities
18:
7:
818:"IMA–CNMNC approved mineral symbols"
719:-like texture. Its hardness on the
1138:"The Crystal Structure of Dickite"
14:
541:Chemical composition of dickite:
378:. It has the same composition as
2254:
2106:
1136:Newnham RE, Brindley GW (1956).
696:substantially heated along with
598:Dickite was first discovered in
680:alternation of limestones and
496:chemist, was on the island of
1:
1008:Ksanda CJ, Barth TF (1935).
723:is 1.5–2, basically between
1066:"Dickite, a Kaolin Mineral"
780:is a=0.576, b=1, c=1.6135.
669:limestones of southeastern
2317:
1410:Fluorotetraferriphlogopite
1050:(seminar material): 41–52.
2301:Minerals in space group 9
2250:
2162:
2097:
1156:10.1107/S0365110X56002060
1116:10.1346/CCMN.1968.0160106
753:monoclinic crystal system
26:
1064:Ross C, Kerr PF (1931).
1096:Clays and Clay Minerals
979:: 15–27. Archived from
1385:Ferroaluminoceladonite
936:"Dickite Mineral Data"
874:Handbook of mineralogy
822:Mineralogical Magazine
209:Flexible but inelastic
16:Phyllosilicate mineral
1248:10.2138/am-2003-5-612
164:a = 5.150, b = 8.940
98:Strunz classification
762:Van der Waals forces
692:. It was found that
684:, westward regional
312:Measured: 50° to 80°
2296:Monoclinic minerals
2291:Clay minerals group
2261:Minerals portal
2113:Minerals portal
1400:Fluorokinoshitalite
1240:2003AmMin..88..837F
1108:1968CCM....16...41S
843:10.1180/mgm.2021.43
834:2021MinM...85..291W
816:Warr, L.N. (2021).
764:between layers and
708:Physical properties
645:, US; San Juanito,
594:Geologic occurrence
360:chemically composed
108:Dana classification
2286:Aluminium minerals
690:igneous intrusions
267:Optical properties
2268:
2267:
2122:
2121:
1612:Ferripyrophyllite
1455:Manganiceladonite
1310:Aluminoceladonite
1143:Acta Crystallogr.
986:on 5 October 2016
772:coordinated to a
323:
322:
302:δ = 0.005 – 0.006
288:= 1.561 – 1.566 n
284:= 1.561 – 1.564 n
142:
2308:
2259:
2258:
2257:
2149:
2142:
2135:
2126:
2111:
2110:
2109:
1545:Tetraferriannite
1405:Fluorophlogopite
1287:
1280:
1273:
1264:
1259:
1234:(5–6): 837–845.
1218:
1217:
1208:(5–6): 554–562.
1196:
1187:
1186:
1170:
1161:
1160:
1158:
1133:
1120:
1119:
1091:
1082:
1081:
1070:
1061:
1052:
1051:
1045:
1036:
1023:
1022:
1005:
996:
995:
993:
991:
985:
969:
963:Dick AB (1888).
960:
951:
950:
948:
946:
932:
926:
925:
923:
921:
907:
896:
895:
871:
862:
856:
855:
845:
813:
573:
563:
550:
537:
442:Isle of Anglesey
354:named after the
346:
276:Refractive index
258:Specific gravity
232:Satiny to pearly
219:
199:Perfect on {001}
136:
82:
62:
61:(repeating unit)
50:serpentine group
31:
19:
2316:
2315:
2311:
2310:
2309:
2307:
2306:
2305:
2281:Phyllosilicates
2271:
2270:
2269:
2264:
2255:
2253:
2246:
2207:Montmorillonite
2158:
2153:
2123:
2118:
2107:
2105:
2093:
2074:Franklinphilite
2055:
2017:
1989:
1956:
1893:
1854:Montmorillonite
1825:
1757:
1664:
1621:
1597:
1569:
1390:Ferroceladonite
1296:
1294:Phyllosilicates
1291:
1224:
1221:
1198:
1197:
1190:
1172:
1171:
1164:
1135:
1134:
1123:
1093:
1092:
1085:
1068:
1063:
1062:
1055:
1043:
1038:
1037:
1026:
1007:
1006:
999:
989:
987:
983:
967:
962:
961:
954:
944:
942:
934:
933:
929:
919:
917:
909:
908:
899:
884:
869:
864:
863:
859:
815:
814:
810:
806:
749:
710:
698:magmatic waters
596:
590:optical means.
571:
567:
562:
558:
554:
549:
545:
536:
532:
528:
524:
520:
518:
490:
345:
341:
337:
333:
329:
292:= 1.566 – 1.570
291:
287:
283:
217:
165:
135:
81:
77:
73:
69:
65:
60:
59:
47:
45:Phyllosilicates
17:
12:
11:
5:
2314:
2312:
2304:
2303:
2298:
2293:
2288:
2283:
2273:
2272:
2266:
2265:
2251:
2248:
2247:
2245:
2244:
2239:
2234:
2229:
2224:
2219:
2214:
2209:
2204:
2199:
2194:
2189:
2184:
2179:
2174:
2169:
2163:
2160:
2159:
2154:
2152:
2151:
2144:
2137:
2129:
2120:
2119:
2117:
2116:
2102:
2098:
2095:
2094:
2092:
2091:
2086:
2081:
2079:Lennilenapeite
2076:
2071:
2065:
2063:
2061:Stilpnomelanes
2057:
2056:
2054:
2053:
2048:
2043:
2038:
2033:
2027:
2025:
2019:
2018:
2016:
2015:
2010:
2008:Ferrisepiolite
2005:
1999:
1997:
1991:
1990:
1988:
1987:
1982:
1977:
1972:
1966:
1964:
1958:
1957:
1955:
1954:
1949:
1944:
1939:
1934:
1929:
1924:
1919:
1914:
1909:
1903:
1901:
1895:
1894:
1892:
1891:
1886:
1881:
1876:
1871:
1866:
1861:
1856:
1851:
1846:
1840:
1838:
1827:
1826:
1824:
1823:
1818:
1813:
1808:
1803:
1798:
1793:
1788:
1783:
1778:
1776:Brinrobertsite
1773:
1767:
1765:
1759:
1758:
1756:
1755:
1750:
1745:
1740:
1735:
1730:
1725:
1720:
1715:
1710:
1705:
1700:
1695:
1690:
1685:
1680:
1674:
1672:
1666:
1665:
1663:
1662:
1657:
1652:
1647:
1642:
1637:
1635:Bismutoferrite
1631:
1629:
1623:
1622:
1620:
1619:
1614:
1608:
1606:
1599:
1598:
1596:
1595:
1590:
1585:
1579:
1577:
1571:
1570:
1568:
1567:
1565:Yangzhumingite
1562:
1557:
1552:
1547:
1542:
1537:
1532:
1530:Siderophyllite
1527:
1522:
1517:
1515:Polylithionite
1512:
1507:
1502:
1497:
1492:
1487:
1482:
1477:
1472:
1467:
1462:
1457:
1452:
1447:
1442:
1437:
1432:
1427:
1422:
1417:
1412:
1407:
1402:
1397:
1392:
1387:
1382:
1377:
1372:
1367:
1362:
1357:
1352:
1347:
1342:
1337:
1332:
1327:
1322:
1317:
1312:
1306:
1304:
1298:
1297:
1292:
1290:
1289:
1282:
1275:
1267:
1261:
1260:
1220:
1219:
1188:
1162:
1149:(9): 759–764.
1121:
1083:
1053:
1024:
997:
965:"On Kaolinite"
952:
940:webmineral.com
927:
897:
882:
857:
828:(3): 291–320.
807:
805:
802:
770:hydroxyl group
766:hydrogen bonds
751:Dickite has a
748:
745:
709:
706:
618:porous rocks.
595:
592:
576:
575:
565:
552:
517:
514:
489:
486:
466:United Kingdom
349:phyllosilicate
321:
320:
318:
314:
313:
310:
304:
303:
300:
294:
293:
289:
285:
281:
278:
272:
271:
268:
264:
263:
260:
254:
253:
250:
244:
243:
240:
234:
233:
230:
224:
223:
220:
211:
210:
207:
201:
200:
197:
191:
190:
187:
181:
180:
177:
173:
172:
171:Identification
168:
167:
162:
156:
155:
150:
144:
143:
132:
126:
125:
120:
118:Crystal system
114:
113:
110:
104:
103:
100:
94:
93:
90:
84:
83:
63:
53:
52:
42:
38:
37:
33:
32:
24:
23:
15:
13:
10:
9:
6:
4:
3:
2:
2313:
2302:
2299:
2297:
2294:
2292:
2289:
2287:
2284:
2282:
2279:
2278:
2276:
2263:
2262:
2249:
2243:
2240:
2238:
2235:
2233:
2230:
2228:
2225:
2223:
2220:
2218:
2215:
2213:
2210:
2208:
2205:
2203:
2200:
2198:
2195:
2193:
2190:
2188:
2185:
2183:
2180:
2178:
2175:
2173:
2170:
2168:
2165:
2164:
2161:
2157:
2156:Clay minerals
2150:
2145:
2143:
2138:
2136:
2131:
2130:
2127:
2115:
2114:
2103:
2100:
2099:
2096:
2090:
2089:Stilpnomelane
2087:
2085:
2084:Parsettensite
2082:
2080:
2077:
2075:
2072:
2070:
2067:
2066:
2064:
2062:
2058:
2052:
2049:
2047:
2044:
2042:
2039:
2037:
2034:
2032:
2029:
2028:
2026:
2024:
2020:
2014:
2011:
2009:
2006:
2004:
2001:
2000:
1998:
1996:
1992:
1986:
1983:
1981:
1978:
1976:
1973:
1971:
1968:
1967:
1965:
1963:
1959:
1953:
1950:
1948:
1945:
1943:
1940:
1938:
1935:
1933:
1930:
1928:
1925:
1923:
1920:
1918:
1915:
1913:
1910:
1908:
1905:
1904:
1902:
1900:
1896:
1890:
1887:
1885:
1882:
1880:
1877:
1875:
1872:
1870:
1867:
1865:
1862:
1860:
1857:
1855:
1852:
1850:
1849:Ferrosaponite
1847:
1845:
1842:
1841:
1839:
1836:
1832:
1828:
1822:
1819:
1817:
1814:
1812:
1809:
1807:
1806:Lunijianlaite
1804:
1802:
1799:
1797:
1794:
1792:
1789:
1787:
1784:
1782:
1779:
1777:
1774:
1772:
1769:
1768:
1766:
1764:
1760:
1754:
1751:
1749:
1746:
1744:
1741:
1739:
1736:
1734:
1731:
1729:
1726:
1724:
1721:
1719:
1716:
1714:
1711:
1709:
1706:
1704:
1701:
1699:
1696:
1694:
1691:
1689:
1686:
1684:
1681:
1679:
1676:
1675:
1673:
1671:
1667:
1661:
1658:
1656:
1653:
1651:
1648:
1646:
1643:
1641:
1638:
1636:
1633:
1632:
1630:
1628:
1624:
1618:
1615:
1613:
1610:
1609:
1607:
1604:
1600:
1594:
1591:
1589:
1586:
1584:
1581:
1580:
1578:
1576:
1572:
1566:
1563:
1561:
1558:
1556:
1553:
1551:
1550:Trilithionite
1548:
1546:
1543:
1541:
1538:
1536:
1533:
1531:
1528:
1526:
1523:
1521:
1518:
1516:
1513:
1511:
1508:
1506:
1503:
1501:
1498:
1496:
1495:Oxyphlogopite
1493:
1491:
1488:
1486:
1483:
1481:
1478:
1476:
1473:
1471:
1468:
1466:
1463:
1461:
1458:
1456:
1453:
1451:
1450:Luanshiweiite
1448:
1446:
1443:
1441:
1440:Kinoshitalite
1438:
1436:
1433:
1431:
1428:
1426:
1423:
1421:
1418:
1416:
1413:
1411:
1408:
1406:
1403:
1401:
1398:
1396:
1393:
1391:
1388:
1386:
1383:
1381:
1378:
1376:
1373:
1371:
1368:
1366:
1365:Chromphyllite
1363:
1361:
1358:
1356:
1353:
1351:
1348:
1346:
1345:Boromuscovite
1343:
1341:
1338:
1336:
1333:
1331:
1328:
1326:
1323:
1321:
1318:
1316:
1313:
1311:
1308:
1307:
1305:
1303:
1299:
1295:
1288:
1283:
1281:
1276:
1274:
1269:
1268:
1265:
1257:
1253:
1249:
1245:
1241:
1237:
1233:
1230:
1229:
1223:
1222:
1215:
1211:
1207:
1204:
1203:
1195:
1193:
1189:
1184:
1180:
1176:
1169:
1167:
1163:
1157:
1152:
1148:
1145:
1144:
1139:
1132:
1130:
1128:
1126:
1122:
1117:
1113:
1109:
1105:
1101:
1097:
1090:
1088:
1084:
1079:
1076:
1075:
1067:
1060:
1058:
1054:
1049:
1042:
1035:
1033:
1031:
1029:
1025:
1021:(9): 631–637.
1020:
1017:
1016:
1011:
1004:
1002:
998:
982:
978:
975:
974:
973:Mineral. Mag.
966:
959:
957:
953:
941:
937:
931:
928:
916:
912:
906:
904:
902:
898:
893:
889:
885:
883:9780962209734
879:
875:
868:
861:
858:
853:
849:
844:
839:
835:
831:
827:
823:
819:
812:
809:
803:
801:
798:
794:
789:
785:
781:
779:
775:
771:
767:
763:
759:
754:
746:
744:
740:
736:
734:
733:birefringence
730:
726:
722:
718:
713:
707:
705:
703:
699:
695:
691:
687:
683:
679:
678:stratigraphic
674:
672:
668:
667:Pennsylvanian
664:
663:volcanic rock
660:
656:
653:area; and in
652:
648:
644:
640:
635:
632:
628:
624:
619:
616:
612:
609:
605:
601:
593:
591:
587:
585:
581:
566:
553:
544:
543:
542:
539:
515:
513:
511:
507:
503:
499:
495:
494:metallurgical
487:
485:
483:
479:
475:
471:
470:United States
467:
463:
459:
455:
451:
447:
443:
439:
435:
431:
430:type location
426:
424:
419:
417:
413:
409:
405:
401:
397:
393:
389:
385:
381:
377:
373:
369:
365:
361:
357:
356:metallurgical
353:
350:
327:
319:
315:
311:
309:
305:
301:
299:
298:Birefringence
295:
279:
277:
273:
269:
265:
261:
259:
255:
251:
249:
245:
241:
239:
235:
231:
229:
225:
221:
216:
212:
208:
206:
202:
198:
196:
192:
188:
186:
185:Crystal habit
182:
178:
174:
169:
163:
161:
157:
154:
151:
149:
145:
140:
133:
131:
130:Crystal class
127:
124:
121:
119:
115:
111:
109:
105:
101:
99:
95:
91:
89:
85:
64:
58:
54:
51:
46:
43:
39:
34:
30:
25:
20:
2252:
2222:Palygorskite
2176:
2104:
2069:Bannisterite
2023:Pyrosmalites
1912:Borocookeite
1907:Baileychlore
1889:Yakhontovite
1884:Volkonskoite
1874:Swinefordite
1791:Hydrobiotite
1708:Cronstedtite
1639:
1617:Pyrophyllite
1603:Pyrophyllite
1583:Minnesotaite
1520:Preiswerkite
1465:Masutomilite
1430:Hendricksite
1231:
1228:Am. Mineral.
1226:
1205:
1202:Am. Mineral.
1200:
1174:
1146:
1141:
1102:(1): 41–49.
1099:
1095:
1077:
1074:Am. Mineral.
1072:
1047:
1018:
1015:Am. Mineral.
1013:
988:. Retrieved
981:the original
976:
971:
943:. Retrieved
939:
930:
918:. Retrieved
914:
873:
860:
825:
821:
811:
790:
786:
782:
750:
741:
737:
714:
711:
702:algal mounds
694:groundwaters
675:
636:
620:
602:, Island of
597:
588:
577:
540:
519:
502:clay mineral
491:
434:Pant-y-Gaseg
427:
423:hydrothermal
420:
352:clay mineral
325:
324:
152:
134:Domatic (m)
2051:Schallerite
2046:Pyrosmalite
2003:Falcondoite
1975:Chrysocolla
1922:Clinochlore
1879:Vermiculite
1835:vermiculite
1796:Karpinskite
1763:Corrensites
1738:Manandonite
1723:Guidottiite
1713:Fraipontite
1698:Caryopilite
1693:Brindleyite
1688:Berthierine
1670:Serpentines
1650:Hisingerite
1593:Willemseite
1555:Voloshinite
1425:Gorbunovite
1395:Fluorannite
1360:Chernykhite
1330:Balestraite
1080:(1): 34–39.
778:axial ratio
516:Composition
374:and 55.78%
270:Biaxial (+)
252:Transparent
248:Diaphaneity
148:Space group
112:71.01.01.01
2275:Categories
2217:Nontronite
2182:Halloysite
2031:Friedelite
1995:Sepiolites
1962:Allophanes
1947:Pennantite
1932:Donbassite
1859:Nontronite
1844:Beidellite
1781:Corrensite
1718:Greenalite
1703:Chrysotile
1683:Antigorite
1645:Halloysite
1627:Kaolinites
1540:Tainiolite
1525:Roscoelite
1510:Phlogopite
1500:Paragonite
1485:Norrishite
1480:Nanpingite
1470:Montdorite
1445:Lepidolite
1420:Glauconite
1370:Clintonite
1355:Celadonite
1350:Bramallite
1325:Aspidolite
915:MinDat.org
804:References
756:bonds: an
721:Mohs scale
655:St. George
611:limestones
428:Dickite's
388:halloysite
362:of 20.90%
317:References
215:Mohs scale
139:H-M symbol
123:Monoclinic
88:IMA symbol
48:Kaolinite-
2232:Sepiolite
2202:Kaolinite
2197:Imogolite
2187:Hectorite
2167:Allophane
2036:Mcgillite
2013:Sepiolite
1985:Neotocite
1980:Imogolite
1970:Allophane
1937:Gonyerite
1917:Chamosite
1899:Chlorites
1869:Sauconite
1831:Smectites
1816:Saliotite
1811:Rectorite
1771:Aliettite
1753:Pecoraite
1733:Lizardite
1655:Kaolinite
1535:Suhailite
1475:Muscovite
1460:Margarite
1375:Eastonite
1183:223495759
1039:Cruz MD.
867:"Dickite"
852:235729616
747:Structure
647:Chihuahua
615:sandstone
584:muscovite
580:feldspars
506:kaolinite
416:potassium
404:magnesium
392:polymorph
380:kaolinite
366:, 21.76%
364:aluminium
160:Unit cell
2237:Smectite
2227:Saponite
2172:Chlorite
2041:Nelenite
1927:Cookeite
1864:Saponite
1821:Tosudite
1801:Kulkeite
1743:Népouite
1728:Kellyite
1560:Wonesite
1505:Phengite
1490:Orlovite
1380:Ephesite
1315:Anandite
1214:41328124
990:28 March
892:20759166
651:rhyolite
643:Colorado
627:breccias
604:Anglesey
498:Anglesey
396:titanium
372:hydrogen
370:, 1.56%
308:2V angle
218:hardness
205:Tenacity
195:Cleavage
41:Category
2212:Nacrite
2177:Dickite
1952:Sudoite
1786:Dozyite
1748:Odinite
1678:Amesite
1660:Nacrite
1640:Dickite
1415:Garmite
1340:Biotite
1335:Bityite
1256:5174457
1236:Bibcode
1104:Bibcode
830:Bibcode
793:cations
631:anatase
623:Jamaica
510:nacrite
488:History
478:Belgium
462:Germany
454:Jamaica
408:calcium
384:nacrite
368:silicon
347:) is a
326:Dickite
102:9.ED.05
57:Formula
36:General
22:Dickite
2192:Illite
1942:Nimite
1837:family
1605:series
1435:Illite
1320:Annite
1254:
1212:
1181:
945:27 Mar
920:27 Mar
890:
880:
850:
797:anions
774:cation
729:gypsum
682:shales
673:, US.
671:Kansas
600:Almwch
574:13.96%
564:39.50%
551:46.54%
482:Canada
458:France
438:Amlwch
432:is in
412:sodium
386:, and
376:oxygen
238:Streak
228:Luster
137:(same
1575:Talcs
1302:Micas
1252:S2CID
1210:S2CID
1069:(PDF)
1044:(PDF)
984:(PDF)
968:(PDF)
870:(PDF)
848:S2CID
758:ionic
639:Ouray
608:algal
474:Italy
450:China
446:Wales
242:White
222:1.5–2
176:Color
2242:Talc
1833:and
1588:Talc
1179:OCLC
992:2019
947:2019
922:2019
888:OCLC
878:ISBN
795:and
727:and
725:talc
717:clay
659:Utah
582:and
533:(OH)
508:and
480:and
414:and
400:iron
342:(OH)
78:(OH)
1244:doi
1151:doi
1112:doi
838:doi
686:dip
546:SiO
262:2.6
92:Dck
2277::
1250:.
1242:.
1232:88
1206:63
1191:^
1165:^
1140:.
1124:^
1110:.
1100:16
1098:.
1086:^
1078:15
1071:.
1056:^
1046:.
1027:^
1019:20
1012:.
1000:^
970:.
955:^
938:.
913:.
900:^
886:.
872:.
846:.
836:.
826:85
824:.
820:.
657:,
641:,
555:Al
525:Si
521:Al
484:.
476:,
472:,
468:,
464:,
460:,
456:,
452:,
444:,
440:,
436:,
418:.
410:,
406:,
402:,
398:,
382:,
334:Si
330:Al
153:Cc
70:Si
66:Al
2148:e
2141:t
2134:v
1286:e
1279:t
1272:v
1258:.
1246::
1238::
1216:.
1185:.
1159:.
1153::
1147:9
1118:.
1114::
1106::
994:.
977:8
949:.
924:.
894:.
854:.
840::
832::
572:O
570:2
568:H
561:3
559:O
557:2
548:2
535:4
531:5
529:O
527:2
523:2
344:4
340:5
338:O
336:2
332:2
328:(
290:γ
286:β
282:α
280:n
141:)
80:4
76:5
74:O
72:2
68:2
Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
