Titlebook: Impact Tectonics; Christian Koeberl,Herbert Henkel Book 2005 Springer-Verlag Berlin Heidelberg 2005 Deformation.Dike.Economic Ecology.Frac

tornado

書目名稱Impact Tectonics影響因子(影響力)




書目名稱Impact Tectonics影響因子(影響力)學(xué)科排名




書目名稱Impact Tectonics網(wǎng)絡(luò)公開度




書目名稱Impact Tectonics網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Impact Tectonics被引頻次




書目名稱Impact Tectonics被引頻次學(xué)科排名




書目名稱Impact Tectonics年度引用




書目名稱Impact Tectonics年度引用學(xué)科排名




書目名稱Impact Tectonics讀者反饋




書目名稱Impact Tectonics讀者反饋學(xué)科排名

Yag-Capsulotomy

The Mechanics of Pseudotachylite Formation in Impact Eventsf a large meteorite impact. The prevailing opinion among many geologists is that pseudotachylites are formed by friction melting of rocks and/or shearing associated with differential shock compression of adjacent rock types. Several physical studies of friction melting have shown that, in theory, sm

Fatten

等待

鬧劇

The Preliminary Analysis of Polygonal Impact Craters within Greater Hellas Region, Mars on all kinds of celestial bodies that have fractured rigid crusts. They are also found on the Earth (e.g., Meteor Crater, S?derfj?rden). Polygonal craters are thought to have been formed by two possible mechanisms. Simple polygonal craters, such as the square-shaped Meteor Crater, result when the e

使殘廢

resuscitation

abolish

Settings of Meteorite Impact Structures in the Svecofennian Crustal Domain Together with younger (1.5 – 1.8 Ga) transition zones it occupies an area of ~1.56 × 10. km.. The domain unites shield and platform areas including the submerged Baltic Sea. It includes 22 confirmed, 6 possible, and tens of supposed impact structures that survived recurrent erosional epochs during

amputation

Geophysical Investigations of the Siljan Impact Structure — A Short Reviewons indicate an age of 377 Ma. The bedrock geology of the region has recently been re-mapped by the Geological Survey of Sweden in the scale of 1:50 000. There is now complete coverage with airborne geophysics. New maps of the geophysical data have been prepared for this review. In connection with t

經(jīng)典

Mj?lnir Crater as a Result of Oblique Impact: Asymmetry Evidence Constrains Impact Direction and Ang5°) angle from the horizontal. This is substantiated by several diagnostic structural and geophysical signatures related to obliquity and revealed through detailed re-assessment of Mj?lnir’s well-established structure, morphology, and gravity and seismic velocity anomalies. The diagnostic signatures