Titlebook: Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites; Contributions to a S R. L. M. Vissers,A. Nicolas Conference proceedings

意見(jiàn)一致

疲勞

Foregery

時(shí)間等

浮雕

abduction

輕浮思想

Mercantile

Plastic Deformation of Gabbros in a Slow-spreading Mesozoic Ridge: Example of the Montgenèvre Ophiolelting within the sheared gabbros, at temperatures of 850° C or higher, generated augite- and pargasite-bearing leucodioritic magmas which evolved in narrow magmatic conduits and percolated through tec-tonites and actively deforming mylonite zones, to form cross-cutting veins in adjacent less deform

使糾纏

Pre-orogenic High Temperature Shear Zones in an Ophiolite Complex (Bracco Massif, Northern Apennines type 3). Reconstruction of the shear zones into their presumed original orientations suggests that they developed as low- to medium-angle extensional fault zones. This has important implications for the inferred processes of ophiolite generation.

Nutrient