It takes the average reader 6 hours and 40 minutes to read Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association by Felix P. Lesnov
Assuming a reading speed of 250 words per minute. Learn more
The monograph is concerned with results of studies of petrology of mafic-ultramafic massifs as part of the East Sakhalin ophiolite association. It generalizes and interprets a large body of data (mainly original data) on geology, petrography, petrochemistry, and geochemistry of rocks; mineralogy and geochemistry of rock-forming and accessory minerals; chromite and platinum contents, and isotopic age of zircons from rocks of the typical mafic-ultramafic massifs of the East Sakhalin ophiolite association: Berezovka, Shel’ting, Komsomol’sk, and South Schmidt. Gabbroids from the Berezovka massif contain ultramafic xenoliths. Ultramafic rocks are locally cut by gabbroid and pyroxenite veins. Three spatially close but genetically autonomous bodies are distinguished in the structure of the massifs under study: protrusion of upper-mantle restitic ultramafic rocks (harzburgites, lherzolites, and dunites); intrusion of orthomagmatic gabbroids (gabbronorites, gabbro, and norites) that cuts it; and contact-reaction zone, located along the boundaries between gabbroid intrusion and ultramafic protrusion, which consists of hybrid ultramafic rocks (wehrlites, websterites, clinopyroxenites, and their olivine- and plagioclase-containing varieties) and hybrid gabbroids (melano- and mesocratic olivine gabbronorites and gabbro as well as troctolites). The hybrid ultramafic rocks and gabbroids are the product of interaction between mafic melts and restitic ultramafic rocks. Taking into account the later formation of the gabbroid intrusions compared to the ultramafic protrusions, the massifs in question are determined as polygenic. The idea of their polygenic formation is supported by data on the isotopic age of zircons from the Berezovka massif rocks. In this monograph the author develops his earlier proposed concept of polygenic formation of mafic–ultramafic massifs belonging to ophiolite associations. The book addresses a wide circle of petrologists and practicing geologists as well as senior-year students and postgraduates studying problems of mafic-ultramafic magmatism.
Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association by Felix P. Lesnov is 394 pages long, and a total of 100,076 words.
This makes it 133% the length of the average book. It also has 122% more words than the average book.
The average oral reading speed is 183 words per minute. This means it takes 9 hours and 6 minutes to read Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association aloud.
Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association is suitable for students ages 12 and up.
Note that there may be other factors that effect this rating besides length that are not factored in on this page. This may include things like complex language or sensitive topics not suitable for students of certain ages.
When deciding what to show young students always use your best judgement and consult a professional.
Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association by Felix P. Lesnov is sold by several retailers and bookshops. However, Read Time works with Amazon to provide an easier way to purchase books.
To buy Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association by Felix P. Lesnov on Amazon click the button below.
Buy Petrology of Polygenic Mafic-Ultramafic Massifs of the East Sakhalin Ophiolite Association on Amazon