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Manganese humites (alleghanyite, manganhumite, and sonolite) and related phases (leucophoenicite and jerrygibbsite) from Franklin and Sterling Hill, New Jersey, were studied. Solid solution between humite and manganhumite is partially continuous, but expected Mn/Mg solid solutions between alleghanyite and chondrodite, and between sonolite and clinohumite, are discontinuous. Manganese is restricted in leucophoenicite and jerrygibbsite, and calcium is common to both. A "threshold" level of zinc is present in all studied samples, and fluorine is proportional to the Mg-content in Mn-humites, but absent in leucophoenicite and jerrygibbsite. No Mn end-members of the manganese humites were found, and the formation of particular species may depend on complex phase relations involving Mn, Mg, Zn, and other elements.

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Manganese humites (alleghanyite, manganhumite, and sonolite) and related phases (leucophoenicite and jerrygibbsite) from Franklin and Sterling Hill, New...

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  • File Format: PDF
  • File Size: 1.01 MB
  • Pages: 9
  • Language: EN
  • Total Downloads: 67
  • Last Updated: 2 hours ago

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