Titlebook: Early Precambrian Basic Magmatism; R. P. Hall,D. J. Hughes Book 1990 Blackie & Son Ltd 1990 chemistry.classification.formation.geochemistr

無能性

Early Precambrian basic rocks of South America (2.7Ga), Transamazonian (2.0Ga), Urua?uano–Espinhago (1.5–1.1 Ga) and Brasiliano (1.1–0.5 Ga) Cycles (see Wernick, 1981), during which the Precambrian crust progressively accreted. It has been estimated that 80% of the Precambrian of South America had formed by the end of the Transamazonian (Cordani ., 1988).

accrete

Unsaturated-Fat

Ausbildung der Beamten in Brasiliennce; Hoffman, 1988), by the 1.8 Ga Hudsonian orogen. The Rae and Hearne Provinces are separated from the Slave Province to the northwest by the Great Slave Lake shear zone. The Nain Province comprises the western part of the North Atlantic craton (see Chapter 11), along the coastal strip of Labrador.

保守黨

ELATE

Sad570

假

Stefanie Albus,Heinz-Günter Micheelpabyssal and volcanic basic components, ranging in age from early to late Archaean. In addition, early to mid-Proterozoic hypabyssal basic intrusions occur in virtually all of the Archaean cratonic regions, while early to mid-Proterozoic metavolcanic suites occur throughout western central USA (Condie, 1986).

可用

addition

和平主義者