26:
363:
During the solid state alteration process the hydrogen atoms migrate through the crystal structure to the surface, where they combine with oxygen. In the process there is a slight shift in the crystal structure, but the structure remains intact. The vanadium-oxygen bonds have not been broken and the
299:
characteristics of the paramontroseite there seem to be two distinct generations: a primary paramontroseite with good crystalline structure and a product of montroseite oxidation with poor crystalline structure. The paramontroseite found in this region is among the neutral minerals in the mid-range
278:
in red sandstone. It is found in a zone where the sandstone changes color from red to gray. The black paramontroseite cements grains of sand into nodular masses that enclose smaller pyrite masses. The irregular concretionary masses are up to 1 foot (0.30 m) across. Vanadium salts have given a
328:
of montroseite. Paramontroseite seems to be the most common initial product of oxidation of montroseite. The primary difference between the crystal structures of the two minerals is that the oxygen–oxygen distance increases from 2.63Å in montroseite to 3.87Å in paramontroseite due to the loss of
332:
The montroseite, VO(OH), is deposited in crystalline masses in a sandstone matrix by some unknown process. Usually iron occurs in place of some of the vanadium. Oxygen in the air or groundwater then oxidizes the crystallised montroseite at temperatures under 50 °C through the reaction:
283:
in the paramontroseite. When a section is polished the paramontroseite completely fills the gaps between the grains of sand. It is very soft and has a gray color that is slightly lighter than quartz gray. There is strong anisotrophism and many bright multi-colored internal reflections.
510:
have shown that synthetic montroseite VOOH hollow structures can convert topochemically to paramontroseite without altering the size and appearance of the structures. Both forms appear to have potential in lithium-ion batteries as
30:
Outstanding pale brown sharp crystals of the rare mineral paramontroseite, a simple vanadium oxide, from the type locality (Bitter Creek Mine, Long Park, Montrose County, Colorado, United States of
America), on a contrasting dark
863:
The measured chemistry of a microprobe fragment in the gray phase by the RRUFF project gave metals in the ratio: V (82%), Fe (9%), U (4%) and Al (2%), with one metal atom per two oxygen atoms. The lightest phase was
329:
hydrogen in the latter. The vanadium–oxygen distances are also somewhat shorter in paramontroseite than in montroseite, as would be expected when the vanadium is oxidized from +3 to +4 when the hydrogen is removed.
364:
hexagonal close-packed oxygen framework has not been disrupted. In some cases there may be an intermediate "diffuse A" phase. The process by which montroseite is altered to paramontroseite seems analogous to the
279:
greenish coating to the exposed surfaces of these masses. The masses are anomalously radioactive and the surrounding sandstone is weakly radioactive. The radioactivity is mostly caused by tiny specks of
1702:
Changzheng, Wu; Feng, Feng; Jun, Feng; Jun, Dai; Jinlong, Yang; Yi, Xie (2011), "Ultrafast Solid-State
Transformation Pathway from New-Phased Goethite VOOH to Paramontroseite VO2 to Rutile VO2(R)",
463:
they may be unable to degrade them and the cell's well-being may be threatened. However, experiments have shown that nanocrystals of paramontroseite induce cyto-protective autophagy in cultured
1766:
Hailong, Fei; Xiaokun, Ding; Mingdeng, Wei; Kemei, Wei (November 2011), "Facile synthesis of
Montroseite VOOH, Paramontroseite VO2 and V2O3-VO2 carbonaceous core-shell microspheres",
207:, USA, where it was first found. Names in other languages include Paramontroseit (German), paramontroseita (Spanish), парамонтрозеит (Russian) and 副黑钒矿 副黑铁钒矿 (Chinese). Synonyms are
525:(M) is potentially of great value for applications such as intelligent temperature sensors and smart windows. The classic solid state transformation from vanadium precursors to
1970:
Zhou, W; Miao, Y; Zhang, Y; Liu, L; Lin, J; Yang, JY; Xie, Y; Wen, L. (26 April 2013), "Induction of cyto-protective autophagy by paramontroseite VO2 nanocrystals",
507:
231:. The type locality is Bitter Creek Mine, Paradox Valley, Uravan District, Montrose County, Colorado, USA. In the USA it is found in Montrose County, Colorado,
713:
pattern for a Bitter Creek mine sample is 3.39 (100), 2.645 (50), 4.35 (35), 2.213 (35), 1.426 (35), 2.479 (25), 2.179 (25). In this sample the chemistry was:
203:, a related mineral. The name was chosen due to the mineral's paramorphic relationship to the host mineral montroseite. Montroseite is named after
1961:
1824:
208:
2034:
560:
79:
252:
2029:
1950:"From synthetic montroseite VOOH to topochemical paramontroseite VO2 and their applications in aqueous lithium ion batteries"
1941:
The
Georges Bank Monitoring Program 1985: Analysis of Trace Metals in Bottom Sediments During the Third Year of Monitoring
183:
mineral in the
Ramsdellite Group. Synthetic paramontroseite may have applications in medicine, batteries and electronics.
893:
553:
Paramontroseite was first described before 1959. It is a member of the
Ramsdellite Group. It is classified as follows:
1881:
915:
248:
232:
104:
2024:
1937:"Geochemical and Crystallographic Constrains on the Formation of the Vanadium-Uranium Ores of the Colorado Plateau"
471:
89:
518:
204:
996:
Montrose County takes its name from the county seat, Montrose, which is named after the historical novel by Sir
2039:
212:
69:
244:
236:
270:
Paramontrosite has also been found in an outcrop on the Van Irvine Ranch in the
Pumpkin Buttes area of
396:
1979:
1775:
1557:
1555:
1059:
223:
Paramontroseite is associated with montroseite and corvusite. It is found in relatively unoxidized
889:
885:
736:
503:
161:
151:
2003:
1936:
1077:
710:
609:
395:
type. The paramontroseite reacts under neutral or acid conditions to form many compounds such as
292:
240:
200:
416:
1949:
1839:
1201:
1199:
404:
400:
392:
1995:
1957:
1919:
1900:
1820:
1814:
1795:
591:
300:
of vanadium valence (+4) above the primary ore of montroseite (+3) but below minerals such as
124:
1787:
1723:
415:. Paramontroseite may dissolve in slightly alkaline conditions, then combine with Ca to form
412:
1987:
1901:"Geology and Uranium Deposits of the Pumpkin Buttes Area of the Powder River Basin, Wyomong"
1783:
1711:
1685:
1174:
1172:
1067:
877:
604:
256:
224:
52:
391:
Paramontroseite is not stable and is destroyed by weathering, replaced by minerals of the
325:
1991:
1983:
1779:
1063:
896:(KC = 0.393), the NCalc is 2.61 where Ncalc=Dcalc*KC+1, or 2.57 where Ncalc=Dmeas*KC+1.
619:
180:
99:
45:
1099:
1097:
1095:
1093:
1091:
2018:
1081:
456:
373:
2007:
1667:
1600:
1598:
1596:
1594:
997:
460:
949:
939:
495:
479:
452:
296:
264:
111:
1649:
1865:
865:
25:
448:
377:
369:
365:
321:
301:
280:
228:
1999:
1742:
1503:
1501:
1499:
1497:
926:
a = 4.905Å, b = 9.422Å, c = 2.916Å, Z = 4; V = 134.76 Den (Calc) = 4.09.
625:
534:
408:
385:
381:
305:
1243:
1241:
1228:
1226:
1072:
1047:
1860:
1472:
1470:
1468:
881:
499:
475:
291:
have been found in the
Saltwash Sandstone Member of the Upper Jurassic
275:
271:
260:
1935:
Wanty, Richard B.; Fitzpatrick, Joan J.; Goldhaber, Martin B. (1986),
1907:, U.S. Department of the Interior, Geological Survey; Washington, D.C.
1796:"Some Quantitative Aspects of the Oxidation and Reduction of the Ores"
1715:
470:
Montroseite and paramontroseite microspheres have been synthesized by
1004:. Montrose, in Forfarshire, Scotland, is a corruption of the Gailic
629:
526:
451:
is a process of cellular degradation that is essential in preserving
1616:
1561:
1546:
1534:
1459:
1205:
1178:
512:
255:. It has also been reported from locations in the Czech Republic,
1627:
1625:
464:
1954:
Issues in
Chemistry and General Chemical Research: 2011 Edition
1899:
Sharp, W.N.; McKay, E.J.; McKeown, F.A.; White, A.M. (1949),
1743:"A crystal Chemical Study of Montroseite and Paramontroseite"
467:
cells. It is possible that this may have value in therapies.
1323:
1321:
1319:
1282:
1280:
316:
Paramontroseite is a metastable form of vanadium dioxide (VO
1518:
1516:
1399:
776:
A sample from
Matchless mine, Colorado, USA had chemistry:
880:
and black to grayish black in color. Its optical class is
1271:
1259:
1017:
The RRUFF database shows Paramontroseite as radioactive.
287:
Deposits of montroseite (V,Fe)OOH and paramontroseite VO
1247:
1232:
1217:
1573:
1447:
1435:
1423:
1190:
1163:
160:
150:
142:
137:
123:
110:
98:
88:
78:
68:
51:
41:
36:
18:
1724:"The Crystal Chemistry and Mineralogy of Vanadium"
1648:Armbruster, Thomas; Danisi, Rosa Micaela (eds.),
1387:
1026:Some sources simply give the color as "black".
583:Physical properties of Paramontroseite include
545:(M) promises to greatly reduce cost and time.
533:(R) is slow and costly. A transformation from
1741:Evans, Howard T. Jr.; Mrose, Mary E. (1955),
1375:
1363:
1298:
1151:
508:University of Science and Technology of China
8:
1522:
904:Paramontroseite crystal properties include:
1351:
1327:
1310:
1286:
1115:
24:
1127:
1071:
498:. These have been used experimentally as
1816:Exploring Colorado Highways: Trip Trivia
1788:10.1016/j.solidstatesciences.2011.09.009
1617:Paramontroseite – Handbook of Mineralogy
1562:Paramontroseite – Handbook of Mineralogy
1547:Paramontroseite – Handbook of Mineralogy
1535:Paramontroseite – Handbook of Mineralogy
1460:Paramontroseite – Handbook of Mineralogy
1206:Paramontroseite – Handbook of Mineralogy
1179:Paramontroseite – Handbook of Mineralogy
455:of cells. It is often thought that when
1272:Wanty, Fitzpatrick & Goldhaber 1986
1260:Wanty, Fitzpatrick & Goldhaber 1986
1038:
989:
1794:Garrels, R. M.; Pommer, A. M. (1987),
1106:, General Paramontroseite Information.
537:VOOH to synthetic "paramontroseite" VO
15:
1604:
1585:
1507:
1476:
1339:
1103:
967:X-Ray diffraction by intensity (I/Io)
7:
1800:Geological Survey professional paper
1728:Geological Survey professional paper
1438:, Relationship ... to other Species.
1139:
1048:"IMA–CNMNC approved mineral symbols"
209:Inorganic Crystal Structure Database
179:) is a relatively rare orthorhombic
1631:
1607:, Paramontroseite Crystallography.
1488:
1411:
1008:, meaning the hill of the ravine.
295:in the Colorado Plateau. From the
14:
1924:, Ardent Media, GGKEY:NS8KWYGW93Y
970:3.39(1), 2.649(0.5), 4.35(0.35).
664:4 (measured), 4.095 (calculated)
1886:Mineralienatlas - Fossilienatlas
1869:, Hudson Institute of Mineralogy
324:of montroseite. It is formed by
1819:, Exploring America's Highway,
459:encapsulate and trap inorganic
253:Fall River County, South Dakota
227:-type uranium–vanadium ores in
1992:10.1088/0957-4484/24/16/165102
1668:"Paramontroseite Mineral Data"
1491:, Physikalische Eigenschaften.
557:Strunz 8th edition: 4/F.08-30.
506:. Y. Xu and colleagues of the
1:
1722:Evans, Howard T. Jr. (1987),
541:to the desired monoclinic VO
399:and metal vanadates such as
669:Calculated electron density
569:Hey's CIM Reference: 7.12.3
249:McKinley County, New Mexico
233:San Miguel County, Colorado
2056:
2035:Minerals in space group 62
1943:, The US Geological Survey
1918:Smythe Palmer, A. (1882),
1905:Geological Survey Bulletin
1686:"Montroseite Mineral Data"
566:Dana 8th edition: 4.4.11.1
472:hydrothermal carbonization
199:(para), meaning near, and
195:is derived from the Greek
1849:, Mineral Data Publishing
1650:"Paramontroseite R050391"
1376:Garrels & Pommer 1987
1364:Garrels & Pommer 1987
1299:Garrels & Pommer 1987
205:Montrose County, Colorado
23:
1574:Paramontroseite – Mindat
1510:, Calculated Properties.
1448:Paramontroseite – Mindat
1436:Paramontroseite – Mindat
1191:Paramontroseite – Mindat
1164:Paramontroseite – Mindat
884:. It has a sub-metallic
677:Calculated fermion index
1537:, X-ray Powder Pattern.
1523:Armbruster & Danisi
1166:, Other Language Names.
894:Gladstone–Dale relation
274:, USA, associated with
213:Powder Diffraction File
1847:Handbook of Mineralogy
1813:Heim, Michael (2007),
1684:Barthelmy (b), David,
1479:, Physical Properties.
1462:, Physical Properties.
1424:Changzheng et al. 2011
1352:Evans & Mrose 1955
1328:Evans & Mrose 1955
1311:Evans & Mrose 1955
1287:Evans & Mrose 1955
1116:Evans & Mrose 1955
1052:Mineralogical Magazine
685:Calculated boson index
624:82.94 gm (61.42%
563:10th edition: 4.DB.15a
245:Apache County, Arizona
146:Black to grayish black
2030:Orthorhombic minerals
1956:, ScholarlyEditions,
1948:Xu, Y. (2012-01-09),
1750:American Mineralogist
1588:, Optical Properties.
1564:, Optical Properties.
444:Possible applications
237:Mesa County, Colorado
80:Strunz classification
1768:Solid State Sciences
1002:A Legend of Montrose
320:) that results from
259:, Argentina and the
1984:2013Nanot..24p5102Z
1802:, Govt. Print. Off.
1780:2011SSSci..13.2049F
1730:, Govt. Print. Off.
1634:, Kristallographie.
1400:Hailong et al. 2011
1313:, pp. 870–872.
1301:, pp. 158−159.
1073:10.1180/mgm.2021.43
1064:2021MinM...85..291W
1046:Warr, L.N. (2021).
876:Paramontroseite is
521:vanadium dioxide VO
504:lithium-ion battery
90:Dana classification
1193:, Type Occurrence.
1152:Smythe Palmer 1882
959:Space group number
711:powder diffraction
293:Morrison Formation
263:uranium mine near
241:Emery County, Utah
2025:Vanadium minerals
1963:978-1-4649-6334-6
1861:"Paramontroseite"
1840:"Paramontroseite"
1826:978-0-9777301-0-0
1774:(11): 2049–2054,
1716:10.1021/jp109967j
1666:Barthelmy, Dave,
1450:, Classification.
1248:Sharp et al. 1949
1233:Sharp et al. 1949
1218:Sharp et al. 1949
974:
973:
934:0.5205:1:0.3094.
912:Crystal structure
859:
858:
772:
771:
700:
699:
592:Empirical formula
211:(ICSD) 22303 and
170:
169:
2047:
2010:
1966:
1944:
1931:
1930:
1929:
1914:
1913:
1912:
1895:
1894:
1893:
1882:"Paramontroseit"
1880:Schorn, Stefan,
1876:
1875:
1874:
1856:
1855:
1854:
1844:
1835:
1834:
1833:
1809:
1808:
1807:
1790:
1762:
1761:
1760:
1747:
1737:
1736:
1735:
1718:
1704:J. Phys. Chem. C
1698:
1697:
1696:
1680:
1679:
1678:
1662:
1661:
1660:
1635:
1629:
1620:
1614:
1608:
1602:
1589:
1583:
1577:
1571:
1565:
1559:
1550:
1544:
1538:
1532:
1526:
1520:
1511:
1505:
1492:
1486:
1480:
1474:
1463:
1457:
1451:
1445:
1439:
1433:
1427:
1421:
1415:
1409:
1403:
1397:
1391:
1388:Zhou et al. 2013
1385:
1379:
1373:
1367:
1361:
1355:
1349:
1343:
1337:
1331:
1325:
1314:
1308:
1302:
1296:
1290:
1284:
1275:
1269:
1263:
1257:
1251:
1245:
1236:
1230:
1221:
1215:
1209:
1203:
1194:
1188:
1182:
1176:
1167:
1161:
1155:
1149:
1143:
1137:
1131:
1125:
1119:
1113:
1107:
1101:
1086:
1085:
1075:
1043:
1027:
1024:
1018:
1015:
1009:
994:
909:
908:
781:
780:
718:
717:
605:Chemical formula
588:
587:
502:materials for a
427:+ 2OH + Ca → CaV
397:vanadyl vanadate
346:
345:
341:
257:Mendoza Province
225:Colorado Plateau
58:
57:(repeating unit)
28:
16:
2055:
2054:
2050:
2049:
2048:
2046:
2045:
2044:
2015:
2014:
2013:
1969:
1964:
1947:
1934:
1927:
1925:
1917:
1910:
1908:
1898:
1891:
1889:
1879:
1872:
1870:
1859:
1852:
1850:
1842:
1838:
1831:
1829:
1827:
1812:
1805:
1803:
1793:
1765:
1758:
1756:
1745:
1740:
1733:
1731:
1721:
1701:
1694:
1692:
1683:
1676:
1674:
1665:
1658:
1656:
1647:
1643:
1638:
1630:
1623:
1619:, Crystal Data.
1615:
1611:
1603:
1592:
1584:
1580:
1572:
1568:
1560:
1553:
1545:
1541:
1533:
1529:
1521:
1514:
1506:
1495:
1487:
1483:
1475:
1466:
1458:
1454:
1446:
1442:
1434:
1430:
1422:
1418:
1414:, p. 1815.
1410:
1406:
1402:, p. 2049.
1398:
1394:
1386:
1382:
1374:
1370:
1362:
1358:
1350:
1346:
1338:
1334:
1326:
1317:
1309:
1305:
1297:
1293:
1285:
1278:
1270:
1266:
1258:
1254:
1246:
1239:
1231:
1224:
1216:
1212:
1208:, Distribution.
1204:
1197:
1189:
1185:
1177:
1170:
1162:
1158:
1150:
1146:
1138:
1134:
1126:
1122:
1114:
1110:
1102:
1089:
1045:
1044:
1040:
1036:
1031:
1030:
1025:
1021:
1016:
1012:
995:
991:
986:
981:
923:Cell dimensions
918:- dipyramidal
902:
900:Crystallography
874:
851:
832:
828:
817:
813:
802:
791:
787:
764:
744:
740:
728:
724:
707:
613:
599:
581:
576:
551:
544:
540:
532:
524:
493:
489:
485:
446:
438:
434:
430:
426:
358:
354:
350:
343:
339:
338:
326:dehydrogenation
319:
314:
290:
221:
215:(PDF) 25-1003.
193:paramontroseite
189:
178:
173:Paramontroseite
132:
130:
64:
56:
55:
32:
19:Paramontroseite
12:
11:
5:
2053:
2051:
2043:
2042:
2040:Oxide minerals
2037:
2032:
2027:
2017:
2016:
2012:
2011:
1978:(16): 165102,
1972:Nanotechnology
1967:
1962:
1945:
1932:
1921:Folk-Etymology
1915:
1896:
1877:
1857:
1836:
1825:
1810:
1791:
1763:
1738:
1719:
1710:(3): 791–799,
1699:
1690:webmineral.com
1681:
1672:webmineral.com
1663:
1654:RRUFF database
1644:
1642:
1639:
1637:
1636:
1621:
1609:
1590:
1578:
1566:
1551:
1539:
1527:
1512:
1493:
1481:
1464:
1452:
1440:
1428:
1426:, p. 791.
1416:
1404:
1392:
1380:
1378:, p. 158.
1368:
1366:, p. 159.
1356:
1354:, p. 874.
1344:
1332:
1330:, p. 872.
1315:
1303:
1291:
1289:, p. 861.
1276:
1264:
1252:
1250:, p. 575.
1237:
1235:, p. 606.
1222:
1220:, p. 605.
1210:
1195:
1183:
1168:
1156:
1154:, p. 545.
1144:
1142:, p. 165.
1132:
1120:
1118:, p. 862.
1108:
1087:
1058:(3): 291–320.
1037:
1035:
1032:
1029:
1028:
1019:
1010:
988:
987:
985:
982:
980:
977:
976:
975:
972:
971:
968:
964:
963:
960:
956:
955:
952:
946:
945:
942:
936:
935:
932:
928:
927:
924:
920:
919:
913:
901:
898:
873:
870:
861:
860:
857:
856:
853:
849:
845:
844:
841:
837:
836:
833:
830:
826:
822:
821:
818:
815:
811:
807:
806:
803:
800:
796:
795:
792:
789:
785:
774:
773:
770:
769:
766:
762:
758:
757:
754:
750:
749:
746:
742:
738:
733:
732:
729:
726:
722:
706:
703:
702:
701:
698:
697:
694:
690:
689:
686:
682:
681:
678:
674:
673:
670:
666:
665:
662:
661:Density (g/cm)
658:
657:
654:
650:
649:
646:
642:
641:
638:
634:
633:
622:
620:Molecular mass
616:
615:
611:
607:
601:
600:
597:
594:
580:
577:
575:
572:
571:
570:
567:
564:
558:
550:
549:Classification
547:
542:
538:
530:
522:
494:-C core-shell
491:
487:
483:
457:autophagosomes
445:
442:
441:
440:
436:
432:
428:
424:
361:
360:
356:
352:
348:
317:
313:
310:
288:
220:
217:
188:
185:
181:vanadium oxide
176:
168:
167:
164:
158:
157:
154:
148:
147:
144:
140:
139:
138:Identification
135:
134:
127:
121:
120:
114:
108:
107:
102:
100:Crystal system
96:
95:
92:
86:
85:
82:
76:
75:
72:
66:
65:
62:
59:
49:
48:
46:Oxide minerals
43:
39:
38:
34:
33:
29:
21:
20:
13:
10:
9:
6:
4:
3:
2:
2052:
2041:
2038:
2036:
2033:
2031:
2028:
2026:
2023:
2022:
2020:
2009:
2005:
2001:
1997:
1993:
1989:
1985:
1981:
1977:
1973:
1968:
1965:
1959:
1955:
1951:
1946:
1942:
1938:
1933:
1923:
1922:
1916:
1906:
1902:
1897:
1887:
1883:
1878:
1868:
1867:
1862:
1858:
1848:
1841:
1837:
1828:
1822:
1818:
1817:
1811:
1801:
1797:
1792:
1789:
1785:
1781:
1777:
1773:
1769:
1764:
1755:
1751:
1744:
1739:
1729:
1725:
1720:
1717:
1713:
1709:
1705:
1700:
1691:
1687:
1682:
1673:
1669:
1664:
1655:
1651:
1646:
1645:
1640:
1633:
1628:
1626:
1622:
1618:
1613:
1610:
1606:
1601:
1599:
1597:
1595:
1591:
1587:
1582:
1579:
1575:
1570:
1567:
1563:
1558:
1556:
1552:
1548:
1543:
1540:
1536:
1531:
1528:
1524:
1519:
1517:
1513:
1509:
1504:
1502:
1500:
1498:
1494:
1490:
1485:
1482:
1478:
1473:
1471:
1469:
1465:
1461:
1456:
1453:
1449:
1444:
1441:
1437:
1432:
1429:
1425:
1420:
1417:
1413:
1408:
1405:
1401:
1396:
1393:
1389:
1384:
1381:
1377:
1372:
1369:
1365:
1360:
1357:
1353:
1348:
1345:
1342:, p. 94.
1341:
1336:
1333:
1329:
1324:
1322:
1320:
1316:
1312:
1307:
1304:
1300:
1295:
1292:
1288:
1283:
1281:
1277:
1274:, p. 20.
1273:
1268:
1265:
1262:, p. 72.
1261:
1256:
1253:
1249:
1244:
1242:
1238:
1234:
1229:
1227:
1223:
1219:
1214:
1211:
1207:
1202:
1200:
1196:
1192:
1187:
1184:
1181:, Occurrence.
1180:
1175:
1173:
1169:
1165:
1160:
1157:
1153:
1148:
1145:
1141:
1136:
1133:
1129:
1128:Barthelmy (b)
1124:
1121:
1117:
1112:
1109:
1105:
1100:
1098:
1096:
1094:
1092:
1088:
1083:
1079:
1074:
1069:
1065:
1061:
1057:
1053:
1049:
1042:
1039:
1033:
1023:
1020:
1014:
1011:
1007:
1003:
999:
993:
990:
983:
978:
969:
966:
965:
961:
958:
957:
953:
951:
948:
947:
944:2/m 2/m 2/m.
943:
941:
938:
937:
933:
930:
929:
925:
922:
921:
917:
914:
911:
910:
907:
906:
905:
899:
897:
895:
891:
887:
883:
879:
871:
869:
867:
854:
847:
846:
842:
839:
838:
834:
824:
823:
819:
809:
808:
804:
798:
797:
793:
783:
782:
779:
778:
777:
767:
760:
759:
755:
752:
751:
747:
745:
735:
734:
730:
720:
719:
716:
715:
714:
712:
704:
695:
692:
691:
688:0.9982793265
687:
684:
683:
680:0.0017206735
679:
676:
675:
671:
668:
667:
663:
660:
659:
655:
652:
651:
647:
644:
643:
639:
636:
635:
631:
627:
623:
621:
618:
617:
614:
608:
606:
603:
602:
595:
593:
590:
589:
586:
585:
584:
578:
573:
568:
565:
562:
561:Nickel-Strunz
559:
556:
555:
554:
548:
546:
536:
528:
520:
516:
514:
509:
505:
501:
497:
481:
477:
473:
468:
466:
462:
461:nanoparticles
458:
454:
450:
443:
422:
421:
420:
418:
414:
410:
406:
402:
398:
394:
389:
387:
383:
379:
375:
374:lepidocrocite
371:
367:
336:
335:
334:
330:
327:
323:
311:
309:
307:
303:
298:
294:
285:
282:
277:
273:
268:
266:
262:
258:
254:
250:
246:
242:
238:
234:
230:
226:
218:
216:
214:
210:
206:
202:
198:
194:
186:
184:
182:
174:
165:
163:
159:
155:
153:
149:
145:
141:
136:
128:
126:
122:
118:
115:
113:
109:
106:
103:
101:
97:
93:
91:
87:
83:
81:
77:
73:
71:
67:
60:
54:
50:
47:
44:
40:
35:
27:
22:
17:
1975:
1971:
1953:
1940:
1926:, retrieved
1920:
1909:, retrieved
1904:
1890:, retrieved
1885:
1871:, retrieved
1864:
1851:, retrieved
1846:
1830:, retrieved
1815:
1804:, retrieved
1799:
1771:
1767:
1757:, retrieved
1753:
1749:
1732:, retrieved
1727:
1707:
1703:
1693:, retrieved
1689:
1675:, retrieved
1671:
1657:, retrieved
1653:
1612:
1581:
1569:
1549:, Chemistry.
1542:
1530:
1484:
1455:
1443:
1431:
1419:
1407:
1395:
1383:
1371:
1359:
1347:
1335:
1306:
1294:
1267:
1255:
1213:
1186:
1159:
1147:
1135:
1123:
1111:
1055:
1051:
1041:
1022:
1013:
1005:
1001:
998:Walter Scott
992:
916:orthorhombic
903:
888:and a black
875:
862:
775:
708:
632:by weight).
582:
552:
517:
496:microspheres
469:
447:
390:
362:
331:
315:
286:
269:
222:
196:
192:
190:
172:
171:
116:
105:Orthorhombic
1888:(in German)
1006:monadh-rois
950:Space group
940:Point group
931:Ratio:a:b:c
892:. From the
693:Radioactive
672:3.85 gm/cc
628:and 38.58%
515:materials.
453:homeostasis
388:processes.
297:diffraction
265:Franceville
201:montroseite
156:Submetallic
112:Space group
2019:Categories
1928:2018-03-20
1911:2018-03-20
1892:2018-03-20
1873:2018-03-15
1866:Mindat.org
1853:2018-03-15
1832:2018-03-20
1806:2018-03-20
1759:2018-03-20
1734:2018-03-20
1695:2018-03-20
1677:2018-03-20
1659:2018-03-20
1340:Evans 1987
866:uranophane
709:The X-ray
574:Properties
519:Monoclinic
480:calcinated
417:simplotite
337:2VO(OH) +
229:sandstones
219:Occurrence
70:IMA symbol
1605:Barthelmy
1586:Barthelmy
1508:Barthelmy
1477:Barthelmy
1140:Heim 2007
1104:Barthelmy
1082:235729616
1034:Citations
979:Endmatter
705:Chemistry
482:to form V
449:Autophagy
405:hummerite
401:hewettite
393:corvusite
378:maghemite
370:maghemite
366:magnetite
322:oxidation
312:Lifecycle
304:(+5) and
302:carnotite
281:coffinite
267:, Gabon.
191:The name
125:Unit cell
2008:45273917
2000:23535229
653:Cleavage
648:brittle
645:Fracture
637:Hardness
626:vanadium
579:Physical
535:goethite
409:pascoite
386:hematite
382:goethite
306:pascoite
276:sulfides
131:b=9.422
119:(no. 62)
94:4.4.11.1
84:4.DB.15a
42:Category
1980:Bibcode
1776:Bibcode
1641:Sources
1412:Xu 2012
1060:Bibcode
882:biaxial
872:Optical
500:cathode
476:sucrose
413:rossite
342:⁄
272:Wyoming
261:Mounana
133:c=2.916
129:a=4.905
53:Formula
37:General
31:matrix.
2006:
1998:
1960:
1823:
1632:Schorn
1489:Schorn
1080:
890:streak
886:luster
878:opaque
835:11.10
656:good
630:oxygen
527:rutile
380:, and
308:(+5).
162:Streak
152:Luster
2004:S2CID
1843:(PDF)
1746:(PDF)
1078:S2CID
984:Notes
954:Pbnm
855:4.82
843:8.26
820:3.00
805:6.12
794:66.9
748:10.5
731:72.5
640:soft
513:anode
351:→ 2VO
166:Black
143:Color
1996:PMID
1958:ISBN
1821:ISBN
962:62.
768:5.0
756:8.8
478:and
465:HeLa
411:and
251:and
197:παρα
187:Name
117:Pbnm
74:Pmto
1988:doi
1784:doi
1712:doi
1708:115
1068:doi
840:FeO
799:SiO
753:FeO
696:no
490:-VO
474:of
435:+ H
423:4VO
355:+ H
175:(VO
2021::
2002:,
1994:,
1986:,
1976:24
1974:,
1952:,
1939:,
1903:,
1884:,
1863:,
1845:,
1798:,
1782:,
1772:13
1770:,
1754:40
1752:,
1748:,
1726:,
1706:,
1688:,
1670:,
1652:,
1624:^
1593:^
1554:^
1515:^
1496:^
1467:^
1318:^
1279:^
1240:^
1225:^
1198:^
1171:^
1090:^
1076:.
1066:.
1056:85
1054:.
1050:.
1000:,
868:.
810:Al
610:VO
596:VO
529:VO
419::
407:,
403:,
384:→
376:→
372:,
368:→
247:,
243:,
239:,
235:,
61:VO
1990::
1982::
1786::
1778::
1714::
1576:.
1525:.
1390:.
1130:.
1084:.
1070::
1062::
852:O
850:2
848:H
831:3
829:O
827:2
825:V
816:3
814:O
812:2
801:2
790:4
788:O
786:2
784:V
765:O
763:2
761:H
743:3
741:O
739:2
737:V
727:4
725:O
723:2
721:V
612:2
598:2
543:2
539:2
531:2
523:2
492:2
488:3
486:O
484:2
439:O
437:2
433:9
431:O
429:4
425:2
359:O
357:2
353:2
349:2
347:O
344:2
340:1
318:2
289:2
177:2
63:2
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