Zobrazeno 1 - 10
of 32
pro vyhledávání: '"D. F. Hewett"'
Autor:
D. F. Hewett, Earl V. Shannon
Publikováno v:
American Journal of Science. :491-506
Autor:
Waldemar T. Schaller, D. F. Hewett
Publikováno v:
American Journal of Science. :29-38
Publikováno v:
Economic Geology. 62:186-206
During a study of hypogene manganese minerals, three silver-bearing manganese oxides were identified in "black calcite" associated with silver ores at the Aurora mine (Treasure Hill), Hamilton, Nevada. Specifically these are: (1) argentian chalcophan
Publikováno v:
Proceedings of the United States National Museum. 73:1-18
Autor:
A. S. Radtke, D. F. Hewett
Publikováno v:
Economic Geology. 62:1-21
The name black calcite has been applied from time to time to a dark gray to black variety of calcite or aragonite in metalliferous ore deposits in the Western States. Most of the material shows curved, roughly rhombic cleavage. The color is due to di
Autor:
D. F. Hewett
Publikováno v:
The Journal of Geology. 28:536-557
The recognition in 1919 of blocks of Madison limestone (Mississippian) overlying beds of the Bridger epoch (middle Eocene) in the McCullock Peak region, 12 miles east of Cody, Wyoming, shows that the overthrust fault recognized by Dake (2) in 1916 is
Autor:
D. F. Hewett
Publikováno v:
Economic Geology. 61:431-461
Review of layered deposits of manganese oxides and carbonates throughout the world indicates that most of the large concentrations are in Precambrian or Tertiary rocks. Iron is generally 30 to 90 times as abundant as manganese in ordinary rocks, wher
Autor:
D. F. Hewett
Publikováno v:
Economic Geology. 67:83-102
This paper is concerned with three of the fairly common, manganese oxide minerals, manganite, hausmannite, and braunite. The study includes the precise determination of the minerals: (1) by X-ray diffraction and (2) spectrographic analyses. Most of t
Autor:
D. F. Hewett
Publikováno v:
Economic Geology. 59:1429-1472
Characteristic minerals are psilomelane, hollandite, cryptomelane, and coronadite, more rarely ramsdellite and pyrolusite. Host rocks are Mn-deficient; 80 percent of examples are middle to late Tertiary layered volcanics. Though deposits are shallow,