By G.W.A. Danen
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18. (A) Impact melt rock from Rochechouart with a large quartz clast bearing a twisted foliated texture. (B)–(D) Detail under the Scanning Electron Microscope of the quartz clast seen in A showing microcrystalline α-quartz spherulites grown from a liquid quartz phase (lechatelierite) in the liquid rock melt, yet preserving a trace of shock induced PDF or planar fractures, the whole indicating that melting of quartz is not due to shock but to thermal overprint of the impact melt upon a moderately shocked quartz clast [LAM 75].
4. 5. Hopkinson Bar test. 6. Hopkinson Bar test. 8. 1. 2. 3. 44. 1. Introduction The field of study of material under extreme loading and application to penetration and impact is classically the scope of dynamic and dynamic-derived research broadly aiming at documenting, understanding and furthermore parametrizing and predicting effects and mechanisms in either projectile, or target, or both, upon impact. The foreseen ultimate purpose is generally either the generation of damage, or the prevention from damage.
The question of strain and damage localization A crucial point is fault prediction. 12). There too, the core of the 30 Materials under Extreme Loadings damaged zone is characterized by near melting conditions resulting in a distinct multilayered texture. Such similarities can be explained. At some distance from the penetration axis, the most important behavior characteristics of the explosive are (i) the dependence of the behavior on pressure and (ii) the influence of damage (microcracking), and the damage-induced instability producing damage and strain localization (faulting).
