Titlebook: Kimberlites, Orangeites, and Related Rocks; Roger Howard Mitchell Book 1995 Springer Science+Business Media New York 1995 Petrogenesis.che

巡洋

書目名稱Kimberlites, Orangeites, and Related Rocks影響因子(影響力)




書目名稱Kimberlites, Orangeites, and Related Rocks影響因子(影響力)學(xué)科排名




書目名稱Kimberlites, Orangeites, and Related Rocks網(wǎng)絡(luò)公開度




書目名稱Kimberlites, Orangeites, and Related Rocks網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Kimberlites, Orangeites, and Related Rocks被引頻次




書目名稱Kimberlites, Orangeites, and Related Rocks被引頻次學(xué)科排名




書目名稱Kimberlites, Orangeites, and Related Rocks年度引用




書目名稱Kimberlites, Orangeites, and Related Rocks年度引用學(xué)科排名




書目名稱Kimberlites, Orangeites, and Related Rocks讀者反饋




書目名稱Kimberlites, Orangeites, and Related Rocks讀者反饋學(xué)科排名

專橫

Suppository

Kimberlites and Orangeites,een termed “micaceous kimberlites” or “group II kimberlites.” The discussion, in conjunction with detailed mineralogical studies described in Chapter 2, will demonstrate conclusively that kimberlites and orangeites cannot be derived from the same parental magma and thus are not genetically related.

手勢(shì)

態(tài)度暖昧

心胸開闊

事先無(wú)準(zhǔn)備

Inflammation

Petrogenesis of Orangeites and Kimberlites,ing from a stance of promoting their own particular bias, be it geophysical, experimental, geochemical, or tectonic, have devised contradictory models for a given magma type. Once introduced, such models are commonly promoted by their originators without impartial reflection on all aspects of the problem or consideration of competing hypotheses.

DAMP

Kimberlites and Orangeites,group I kimberlites, with those of the group of diamond-bearing rocks which, in this work, are termed “orangeites.” The latter rocks have previously been termed “micaceous kimberlites” or “group II kimberlites.” The discussion, in conjunction with detailed mineralogical studies described in Chapter

爆炸

Mineralogy of Orangeites,s, previous studies did not attempt to delineate mineral assemblages and compositional trends which could be used to discriminate between each group of rocks. This chapter is based upon many new analyses of minerals in archetypal kimberlites and orangeites. The study of the latter is far from defini