Titlebook: Basement Tectonics 7; Proceedings of the S Robert Mason Conference proceedings 1992 Springer Science+Business Media Dordrecht 1992 Deformat

Mutter

瘋狂

cinder

暴發(fā)戶

Tectonic Evolution of Northwestern South America “rift and drift” phases of the breakup of Pangea. During latest Cretaceous and into the Paleocene, microplate collision affected the entire South American margin, locally forming a suture. Interactions with the Caribbean and Nazca plates intensified and, starting in Miocene time with a Pliocene pea

Urea508

Ambiguous

prostatitis

小步舞

Fundamental Crustal Lineaments and Transverse Structural Zones in Continental Rifts as kinematic analogues of oceanic transform faults. However, detailed seismic interpretation and structural mapping of transverse zones in the North Sea Rift have revealed a connection between the transverse zones and fundamental basement lineaments in N.W. Europe. Major offsets of the Mesozoic Nor

高貴領(lǐng)導(dǎo)

Tectonic Controls on the Lake Victoria Basinund the craton margins, and intersection among a series of NW-trending strike-slip faults which transect the craton. Casual observation might suggest that the basin was formed by meteorite impact (Saul and Glaholm, 1981), but there is no geologic evidence (i.e., impact breccias, tektites, radial fra

最高點(diǎn)

Basement Extension on the Newfoundland Continental Margin (Canadian East Coast)ower crustal zone and underlies most of the Newfoundland offshore structural elements. A linked system of synthetic and antithetic faults associated with this crustal detachment now borders the structural units of the shelf..The widespread reactivation of pre-existing Precambrian and Paleozoic zones