Abstract
The Macquarie Island ophiolite is an uplifted block of oceanic crust formed at the Australia-Pacific spreading center between 12 and 9 Ma. The sense of motion and geological processes across this plate boundary reflect an evolution from orthogonal spreading through progressively more oblique spreading to the present-day transpressional regime. The crust that makes up the island was formed during an interval of oblique spreading along east-trending spreading segments punctuated by a series of northwest-trending discontinuities. The discontinuities are accommodation zones marked by oblique-slip dextral-normal faults, localized dikes and lava flows, and extensive hydrothermal alteration, indicating that these zones were active near the spreading axis. These features provide a window into the internal structure of oceanic crust generated by oblique spreading.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 125-128 |
| Number of pages | 4 |
| Journal | Geology |
| Volume | 32 |
| Issue number | 2 |
| DOIs | |
| State | Published - Feb 2004 |
| Externally published | Yes |
Keywords
- Discontinuities
- Hydrothermal circulation
- Oblique-slip faults
- Seafloor spreading
- Transfer zones
ASJC Scopus subject areas
- Geology