Pansament / Tectonic - Revoluție? album flac

Complete your Pansament, Tectonic collection.

Pansament is from Brașov Tectonic is from București. Red and black printing. Following a crazy trip by road through Romania in 1991, and the discovery of the local scene, it was decided to release this record and create TAM89. This was the first underground Romanian record ever. Tectonic plays thrashcore and Pansament punk. Matrix, Runout (Side A runout - stamped): MZO 0121/A.

Revoluție? Tectonic, Pansament. Released in red or green cover. Recording information: These tracks were recorded live in 1992 at the Samrock festival, where they won the first prize. Identifiers: Matrix, Runout (Side A Runout - Machine Stamped): MZO 0121/A Matrix, Runout (Side B Runout - Machine Stamped): MZO 0122/A.

Pansament with Tectonic were the first two Romanian bands releasing a split EP for the Western market called "Revolutie?" in 1993 under the French label Tian An Men'91 Records, actually it was the first release of this label and it's a collector's delicatessen. Immediate download of 16-track album in your choice of 320k mp3, FLAC, or just about any other format you could possibly desire. Purchasable with gift card.

The Aravalli Mountain Range is a northeast-southwest trending orogenic belt in the northwest part of India and is part of the Indian Shield that was formed from a series of cratonic collisions. The Aravalli Mountains consist of the Aravalli and Delhi fold belts, and are collectively known as the Aravalli-Delhi orogenic belt. The whole mountain range is about 700 km long.

Tectonic evolution of the Transantarctic Mountains. The tectonic evolution of the Transantarctic Mountains appears to have begun when Antarctica broke away from Australia during the late Cretaceous and is ongoing, creating along the way some of the longest mountain ranges (at 3500 kilometers) formed by rift flank uplift and associated continental rifting. The Transantarctic Mountains (TAM) separate East and West Antarctica

The Early Paleozoic tectonic regime in southwestern Gondwana involved a period of rifting during the Cambrian which affected the southern margin of the supercontinent, while at the same time the western margin experienced a compressional setting that saw the accretion of several exotic terranes. The large, continuous passive margin produced during this rifting event led to the formation of several associated basins Collision of Exotic Terranes.