The breakup of Laurasia to form the Northeast Atlantic Realm disintegrated an
inhomogeneous collage of cratons sutured by cross-cutting orogens. Volcanic rifted margins …

Tectonics and erosion are the driving forces in the evolution of mountain belts, but the
identification of their relative contributions remains a fundamental scientific problem in …

Following an outline of Scandinavian Caledonide tectonostratigraphy, tracing the
Neoproterozoic, Baltoscandian, passive margin of Baltica outboard into the suspect, Iapetus …

在华北, 华南板块碰撞期间, 郯庐断裂带究竟是何种边界仍是没有解决的重大地学问题,
许多学者对此提出了不同的构造解释模式. 关于郯庐断裂的平移距离仍存在着较大的分歧与有待 …

None of the existing models for calc-alkaline “Late Granite”(Siluro–Devonian) genesis in the
metamorphic Caledonian orogenic belt of Ireland and Scotland fully explains their spatial …

Detailed structural geological and related studies were carried out in a number of critical
areas in the Proterozoic basement of eastern Egypt to resolve the structural pattern at a …

Neoproterozoic tectonics is dominated by the amalgamation of the supercontinent Rodinia
at ca. 1.0 Ga, its breakup at ca. 0.75 Ga, and the collision between East and West …

A regional grid of multichannel seismic reflection profiles records the Late Palaeozoic
structure and tectonic development of the south-western Barents Sea. A 300 km wide rift …

Striking similarities between the late Mesoproterozoic–Early Paleozoic record of Avalonia
and the Late Paleozoic–Cenozoic history of western North America suggest that the North …

The late Silurian to mid-or late Devonian interval in the Caledonides was a period
dominated, sequentially, by sinistral transpression, strike-slip and transtension during the …