Titlebook: Earthquakes at North-Atlantic Passive Margins: Neotectonics and Postglacial Rebound; S?ren Gregersen,Peter W. Basham Book 1989 Kluwer Acad

猛烈責(zé)罵

Narrative

聯(lián)想記憶

tangle

The New Party: Ideal and Reality (to 1906),th Atlantic plate boundaries; 4) Disparities between spreading rates and continental separation, and 5) Mantle diapirism causing crustal doming, generally leading to rifting and vulcanism..Today only about 20% of the margin presents geological indications of continued deformation, symmetrically dist

不透明

窩轉(zhuǎn)脊椎動物

elucidate

Intervertebral Disc Calcification, good fit of the data to a straight line, with most points falling within a meter of predicted altitude. Because the profile is so straight over a very long distance and because it represent varying rates of ice retreat, no uplift is indicated for this area for at least 2000 years, until after 14,00

Ambulatory

Electrostatics. Electric Currents,ust represent an extraordinary episode in the regional déglaciation. The interaction of crustal deweighting and residual hydrous overpressuring, allied with long-term tectonic compression, has created a unique upper crustal stress state, and triggered some fault styles that have no present-day analo

核心

不在灌木叢中