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- W2990081144 abstract "Metamorphic rocks can be thought of as flight recorders, black boxes recovered from the wreckage of an orogen that tell us something of that orogen's history – primarily the pressure or depth (P), temperatures (T), and times (τ) of the journey. P, T and τ are linked by the physics of heat transfer and the thermodynamics and kinetics of possible transformations in the rocks mass. For a simplified one-dimensional rock mass, this relation can be visualized as a surface in depth(= P)–T–τ space (Fig. 12.1 (A)). P–T–τ paths of rocks are lines on this surface. Tectonic histories (P–τ paths) studied by the structural geologist, P–T loops determined by the metamorphic petrologist, and the T–τ histories examined by the geochronologist are all projections of the P–T–τ path onto the appropriate surface (Fig. 12.1(B))." @default.
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- W2990081144 date "1991-02-22" @default.
- W2990081144 modified "2023-09-29" @default.
- W2990081144 title "An essay on metamorphic path studies or Cassandra in <i>P–T–τ</i> space" @default.
- W2990081144 doi "https://doi.org/10.1017/cbo9780511564444.014" @default.
- W2990081144 hasPublicationYear "1991" @default.
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