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- W2003564095 abstract "Abstract The strain and strain partitioning in the Helvetic thrust belt are analysed in order to determine their variation across the belt from the external, thin-skinned portion to the internal, thick-skinned portion, and in order to begin the detailed mechanical analysis of the entire fold-and-thrust belt. Coarse-grained limestones of Jurassic and Cretaceous age were chosen for analysis because they can be traced from the external to the internal zones. The strain within a bed is partitioned into three components: transgranular (pressure solution, microfaults, veins), twinning, granular and intragranular, exclusive of twinning (crystal-plasticity, associated with recrystallization). Transgranular strain was very important in the early history of the Helvetic nappes giving way to twinning at a later stage under tectonic burial. Twinning strain was early in the Infrahelvetic complex, giving way to intracrystalline deformation at the later stage of burial. The transition from transgranular- to intragranular-dominated strain occurred at a vitrinite reflectance value of 3.5%, significantly below the greenschist grade of metamorphism. In a large-scale fold at the leading edge of the Helvetic nappes, transgranular strains were associated with the buckling stage of the fold and twinning occurred during fold-tightening. In more internal parts of the Helvetic nappes twinning strains are also late with regard to transgranular strains, but here their pattern corresponds to the regional finite strain pattern. In the internal zone, the Infrahelvetic complex, twinning seems to have been an early event and records an initial layer-parallel shortening, followed by regional internal deformation with intragranular strains." @default.
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- W2003564095 date "1984-01-01" @default.
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- W2003564095 title "Strain partitioning in the Helvetic thrust belt of eastern Switzerland from the leading edge to the internal zone" @default.
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- W2003564095 doi "https://doi.org/10.1016/0191-8141(84)90079-8" @default.
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