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The pumpellyite mineral series

Published online by Cambridge University Press:  14 March 2018

D. S. Coombs
D. S. Coombs*
Affiliation:
Geological Department, University of Otago, New Zealand
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Extract

The bluish-green epidote-like mineral, pumpellyite, was first described by Palache and Vassar (1925) from the copper-bearing amygdaloidal lavas of the Lake Superior region. It has since been reported from many parts of the world in rocks which have undergone low grades of metamorphism, especially types such as amygdaloidal spilites and diabases (Burbank, 1927; Waldmann, 1934; Tsuboi, 1936; Quitzow, 1935, 1936; Klein, 1939; Laeroix, 1942; Seether, 1942; Zavaritsky, 1944:; Korzhinsky, ]944; de Roever, 1947a, b; Kvasha, 1950) and in glaueophane-schists and even eclogites in which pumpellyite is often associated with lawsonite (Irving, Vonsen, and Gonyer, 1932; Quitzow, 1935, 1936 ; Lacroix, 1942 ; Switzer, 1945 ; de Roever, 1947a, b, 1950). W. P. de Roever (1947a, 1950) has suggested a pumpellyitic facies of metamorphism as a lower-grade equivalent of his lawsoniteglaucophane subfacies, characterized by high confining pressure, but subordinate shearing stress and thermal influence, and passing into unmetamorphosed rocks.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 30 , Issue 221 , June 1953 , pp. 113 - 135
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1953

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References

Amies, (A. C), 1950. An intrusion of porphyrite near Waihao Forks, South Canterbury. Trans. Roy. Soc. N.Z., vol. 78, pp. 271–279.Google Scholar
Burbank, (W. S.), 1927. Additional data on the properties of pumpellyite, and its occurrence in the republic of Haiti, West Indies. Amer. Min., vol. 12, pp. 421–424. [M.A. 3-454.]Google Scholar
Foote, (A. E.), 1873. On zonochlorite, a new hydrous silicate from Neepigon Bay, north shore of Lake Superior, B.A. Proc. Amer. Assoc. Adv. Sci., Dubuque meeting, Aug. 1872, pp. 65–66.Google Scholar
Hawes, (G. W.), 1875. On zonochlorite and chlorastrolite. Amer. Journ. Sci., ser. 3, vol. 10, pp. 24–26.Google Scholar
Hutton, (C. O.), 1937. An occurrence of the mineral pumpellyite in the Lake Wakatipu region, western Otago, New Zealand. Min. Mag., vol. 24, pp. 529–533.Google Scholar
Hutton, (C. O.) 1940. Metamorphism in the Lake Wakatipu region, western Otago, New Zealand. N.Z. Dept. Sci. Ind. Res. Geol. Mem., no. 5.Google Scholar
Irving, (J.), Vousen, (M.), and Gonyer, (F. A.), 1932. Pumpellyite from California. Amer. Min., vol. 17, pp. 338–342. [M.A. 5-233.]Google Scholar
Ito, (T.), 1947. The structure of epidote (HCa2(Al,Fe)Al2Si3O13). Amer. Min., vol. 32, pp. 309–321. [M.A. 10-212.]Google Scholar
Ito, (T.) 1950. X-ray studies on polymorphism. Tokyo. [M.A. 11-308.]Google Scholar
Klein, (I.), 1939. Microcline in the native copper deposits of Michigan. Amer. Min., vol. 24, pp. 643–650. [M.A. 8-16.]Google Scholar
Kokzhinsky, (D. S.), 1944. An abyssophobe mineral pumpellyite in the rocks of the Mount Blagodat and the Turya river and on the factor of the transformation energy. Bull. Aead. Sci. URSS, Sér. Géol., no. 5, 87–91. (Russian with English summary). [M.A. 9-210.]Google Scholar
Kvasha, (L. G.), 1950. Pumpellyite from the agglomerate of the ore-free pyroclastic formation of the village of Levikha in middle Urals. Mém. Soc. Russe Min., sér. 2, vol. 79, pp. 142–146. [M.A. 11405.]Google Scholar
Lacroix, (A.), 1887. Études critiques de minéralogie. Bull. Soc. Franç. Min., vol. 10, pp. 142–152.Google Scholar
Lacroix, (A.) 1942. Les glaucophanites de la Nouvelle-Calédonie et les roches qui les accompagnent, leur composition et leur genèse. Mém. Acad. Sci. Inst. France, vol. 65 (for 1941), 103 pp. [M.A, 9-274.]Google Scholar
Munteanu-Murgoci, (G.), 1900. Über die Einschlüsse von Grant-Vesuvianfels in dem Serpentin des Parîngu-Massiv's. Bull. Soc. Sci. Bukarest, vol. 9, pp. 568–612, 764-831. Also Inaug.-Diss. Univ. München, 1901, especially pp. 31, 67-68.Google Scholar
Nel, (H. J.), Strauss, (C. A.), and Wickman, (F. E.), 1949. Lombaardite, a new mineral from the Zaaiplaats tin mine, central Transvaal. Mem. Geol. Surv. South Africa, no. 43, pp. 45–53. [M.A. 11-127.]Google Scholar
Norin, (R.), 1941. Tillämpning av termisk analys på leror och vattenhaltiga mineral. Geol. För. Förh. Stockholm, vol. 63, pp. 203–228.Google Scholar
Palache, (C.) and Vassar, (H. E.), 1925. Some minerals of the Keweenawan copper deposits: pumpellyite, a new mineral; sericite; saponite. Amer. Min., vol. 10, pp. 412–418. [M.A. 3-8.]Google Scholar
Quitzow, (H. W.), 1935. Diabas-Porphyrite und Glaucophangesteine in der Trias von Nordkalabrien. Nachr. Gescll. Wiss. Göttingen, math.-phys. KI., Fachgr. IV, N.F., vol. 1, pp. 83–118.Google Scholar
Quitzow, (H. W.) 1936. Pumpellyit, tin häufiges Hydrothermal- und Sekundärmineral in basichen Gesteinen. Zentral. Min., Abt. A, pp. 39–46. [M.A. 6-429.]Google Scholar
Reed, (J. J.), 1950. Spilites, serpentinites and associated rocks of the Mossburn district, Southland. Trans. Roy. Soc. N.Z., vol. 78, pp. 106–126.Google Scholar
Roever, (W. P. de), 1947a. Igneous and metamorphic rocks in eastern central Celebes. Geol. Expl. in the island of Cclebes (Brouwer, H. A.), Amsterdam, pp. 65–173. [M.A. 11-200.]Google Scholar
Roever, (W. P. de) 1947b. Occurrences of the mineral pumpellyite in eastern Borneo. Bull. Bureau Mines and Geol. Surv. Indonesia, vol. 1, pp. 16–17. [M.A. 10-273.]Google Scholar
Roever, (W. P. de) 1950. Preliminary notes on glaucophane-bearing and other crystalline schists from south east Celebes, and on the origin of glaucophane-bearing rocks. K. Nederl. Akad. Wetensch., vol. 53, pp. 1455–1465.Google Scholar
Sæther, (E.), 1942. Funn av pumpellyitt i bergarter fra Oslofeltet. Norsk Geol. Tidsskr., vol. 21 (for 1941), pp. 294–295. [M.A. 9-211.]Google Scholar
Sobolev, (V. S.), 1947. A new discovery of pumpellyite (lotrite). Min. Journ. Geol. Soc. Lvov, no. 1.Google Scholar
Söhnge, (P. G.), 1945. The structure, ore genesis and mineral sequence of the cas: siterite deposits of the Zaaiplaats tin mine, Potgietersrust district, Transvaal. Trans. Geol. Soc. South Africa, vol. 47 (for 1944), pp. 157–181. [M.A. 10-233.]Google Scholar
Switzer, (G.), 1945. Eclogite from the Californian glaucophane schists. Amer. Journ. Sci., vol. 243, pp. 1–8. [M.A. 9-168.]Google Scholar
Tsuboi, (S.), 1936. Petrological notes (11). Pumpellyite from Asahine, Tukikawa- mura, Titibu-gôri, Saitama prefecture. Japanese Journ. Geol. Geog., vol. 13, p. 333. [M.A. 7-30.]Google Scholar
Turner, (F. J.), 1939. In Williamson, (J. W.). The geology of the Naseby sub-division. N.Z. Geol. Surv. Bull., no. 39.Google Scholar
Villiers, (J. E. de), 1941. Optical properties and crystallography of zoned pumpcllyite from the Witwatersrand. Amer. Min., vol. 26, pp. 237–446. [M.A. 8- 338.]Google Scholar
Waldmann, (L.), 1934. Pumpellyit aus Steiermark und Finnisch-Lappland. Tsehermaks Min. Petr. Mitt., vol. 45, pp. 92–93. [M.A. 5479.]Google Scholar
Whitney, (J. D.), 1847. Description and analysis of three minerals from Lake Superior. Journ. Nat. Hist. Boston, vol. 5, p. 488.Google Scholar
Wickman, (F. E.), 1947. The crystal structure of lawsonite, CaAl2(Si2O7)(OH)2.H2O. Arkiv Kemi, Min. Geol., vol. 25A, no. 2, 7 pp. [M.A. 10-338.]Google Scholar
Zavaritsky, (V. A.), 1944. Pumpellyite in the green-stone rocks of the Uchaly region at the south Urals. Bull. Acad. Sci. URSS, Sér. Géol., no. 5, pp. 92–97. [M.A. 9-211.]Google Scholar