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The Formation of Hydrothermal Cookeite in the Breccia Pipes of the Ardlethan Tin Field, New South Wales, Australia
| Content Provider | Semantic Scholar |
|---|---|
| Author | Ren, Shuang K. Eggleton, Richard A. Walshe, Eno John L. |
| Copyright Year | 1988 |
| Abstract | Cookeite, a diltrioctahedral chlorite, occurs in the breccia pipes of the Ardlethan tin field, New South Wales, Australia. Cookeite formed as a late-stage, low-temperature (150 to 190"C) hydrothermal product in pore spaces in breccias which host disseminated cassiterite and sulfide mineralization. The coupled substrtution Al + Li = Si + ! results in high Si and low Li and Al contents which consequently results in a low occupancy of octahedral positions. Refined cell parameters are a 5.158(l), b 8.929(l), c r4.232Q) A, B 96.91(1)". |
| Starting Page | 407 |
| Ending Page | 412 |
| Page Count | 6 |
| File Format | PDF HTM / HTML |
| Volume Number | 26 |
| Alternate Webpage(s) | http://rruff.info/uploads/CM26_407.pdf |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |