| Reference Type | Journal (article/letter/editorial) |
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| Title | Further Studies in Chert. I |
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| Journal | Geological Magazine |
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| Authors | Sargent, H. C. | Author |
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| Year | 1929 (September) | Volume | 66 |
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| Issue | 9 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800105308 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 245711 | Long-form Identifier | mindat:1:5:245711:0 |
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| GUID | 0 |
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| Full Reference | Sargent, H. C. (1929) Further Studies in Chert. I. Geological Magazine, 66 (9) 399-413 doi:10.1017/s0016756800105308 |
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| Plain Text | Sargent, H. C. (1929) Further Studies in Chert. I. Geological Magazine, 66 (9) 399-413 doi:10.1017/s0016756800105308 |
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| In | (1929, September) Geological Magazine Vol. 66 (9) Cambridge University Press (CUP) |
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| Abstract/Notes | Dr. F. W. Clarke truly observes in regard to the origin of chert: “No one process can account for all the occurrences of amorphous and cryptocrystalline silica, and each locality must be studied in the light of its own evidence.” (Data of Geochemistry, 1916, p. 544.) |
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