Geochemical Characteristics of Igneous Rocks of the Nizhnetaezhny Ore District (North Primorye)

• Published in: IOP Conference Series: Earth and Environmental Science
• Main Authors: Medvedev, E I, Ivin, V V
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: IOP Publishing 2022
• Subjects: Chukchi
• Online Access: http://dx.doi.org/10.1088/1755-1315/988/5/052058; https://iopscience.iop.org/article/10.1088/1755-1315/988/5/052058; https://iopscience.iop.org/article/10.1088/1755-1315/988/5/052058/pdf

Abstract The article discusses the features of the geological structure and composition of the magmatic rocks of the Nizhnetaezhny ore district (North Primorye). It ncludes the East Sikhote-Aligna Volcano-plutonic belt (ESAVPB) and is located in the transition zone Continent Ocean. ESAVPB is the typomorphic link of the East Asian Occinno-Continental Volcanogenic, reconstructed by A. I. Khanchuk as an oversumbays. Other links are known as the Okhotsko-Chukchi, Busan and Southeast Chinese belts. To determine the age of the magmatic arrays, the NTOD selected from the two most representative intrusive bodies of the node of the Malinovsky and Berezovsky massives, between them the main mass of ore mineralization is located. The determination of the ages of the K-Ar method is shown that quartz diorites were formed in Paleocene (64 ± 1 million years), and biotite porphyrene granites in Eocene (47 ± 2 million years). It was previously assumed that the Malinovsky massive is a typical representative of Primorsky, and Berezovsky and the Zavodskoy - Samarka or Bogopolskaya volcanic Plutonic Comlex. Considering that some definitions show (62 ± 1 million years) and characterize porphyry dacites in the Exocontact attacked of the Berezovsky massive, and in the bottom of the incision of the bogopolskaya suites, the lumpy tuffs of rhyolitic and touff-conglomerates contain retalized and half-rolled fragments of the myarol granites common in the Primorsky complex, we can conclude About accessories Malinovsky and Berezovsky massive to the Samarkinskiy complex. In favor of such a conclusion, the determination of the age of monzodiorite (64 ± 1 million years) and pyroxene diorites (57 ± 2 million years) of the Malinovsky massive, which are consistent with the refined rates of the age of the Samargna suite, are appropriate.