Titlebook: Oceanic Basalts; P. A. Floyd Book 1991 Blackie and Son Ltd 1991 environment.formation.gas.geology.igneous rock.mineral.mineralogy.petrogen

热情赞扬

Pacific ocean crustrgest and fastest moving plate, the Pacific plate, in addition to the smaller Nazca, Cocos, Rivera, Juan de Fuca, Gorda and Explorer plates, three so-called micropiates (Galapagos, Easter and Juan Fernandez), plus portions of neighbouring plates in the south and south-west Pacific (Figure 11.1). Des

值得尊敬

Indian ocean crust detailed petrographic observations and mineral chemistry. The mineralogical aspects and the magmatic processes envisaged can be considered as adjunct topics to Chapters 5 and 7, respectively, in Part II. The first section considers the consequences of the existence of magmatic lineages, which are p

腐烂

staging

Oceanic peridotitest the island was not of volcanic origin. Around the turn of the century peridotites broadly similar to those on St. Paul’s rocks were found as basalt- and kimberlite-borne xenoliths in ocean basins and on continental crust. Indeed it was the correlation between the seismic properties of such ultrama

Instrumental

UTTER

Introduction and the ophiolite modely to land-bound lay people the great depth of the oceans, the fundamental differences between continents and oceans, and the constant renewal of the ocean floor by seafloor spreading and subduction, when their concepts are bounded by a wrinkled sea surface viewed from the air. In the early nineteenth century such ideas lay beyond everyone’s grasp.

捕鲸鱼叉

slow-wave-sleep

Metamorphic and hydrothermal processes: basalt—seawater interactions changed, and the resulting metamorphosis and evolution of the oceanic crust as it ages and passes from its place of origin at the accreting plate margin to its eventual return to the mantle at subduction zones.

使服水土

Back-arc basinssis in many tectonic settings. The study of magmatism at destructive plate boundaries provides important information about the scale of crustal recycling, which may in time influence our understanding of the evolution of the crust and mantle.

reception