Lower Moscovian Limestones of the Bogdashan Range (NW China) as an
Por um escritor misterioso
Descrição

a) Location of the study area in the Central Asian Orogenic Belt (modi

Bo WANG, Professor, PhD, Nanjing University, Nanjing, NJU, Department of Earth Science

Lower Moscovian Limestones of the Bogdashan Range (NW China) as an Indicator of Cessation of Arc Magmatism in the Junggar Region

Yuriy BISKE, Professor (Full), Doctor Geol.-miner. Sciences, Saint Petersburg State University, Saint Petersburg, SPBU, Earth Sciences

Representative photographs of hand specimens and thin sections. (a) K-3

PDF) Lower Moscovian Limestones of the Bogdashan Range (NW China) as an Indicator of Cessation of Arc Magmatism in the Junggar Region

Facies architecture of a subaqueous volcano–sedimentary succession on Bogda Mountains, NW China—Evidence of extension in Late Carboniferous - Memtimin - 2020 - Geological Journal - Wiley Online Library

Paleozoic collisional belt of the South Tien Shan: A review - ScienceDirect

PDF] Brachiopods from the Valdeteja Formation (Pennsylvanian; Cantabrian Mountains, NW Spain)

Paleozoic multiple accretionary and collisional tectonics of the Chinese Tianshan orogenic collage - ScienceDirect

Facies architecture of a subaqueous volcano–sedimentary succession on Bogda Mountains, NW China—Evidence of extension in Late Carboniferous - Memtimin - 2020 - Geological Journal - Wiley Online Library

Lower Moscovian Limestones of the Bogdashan Range (NW China) as an Indicator of Cessation of Arc Magmatism in the Junggar Region

Upper Triassic‒Middle Jurassic resedimented toe-of-slope and hemipelagic basin deposits in the Dinaridic Ophiolite Belt, Zlatar Mountain, SW Serbia
Lower Moscovian limestones of the Bogdashan Range (NW China) as an indicator of cessation of arc magmatism in the Junggar region - Alexeiev - Стратиграфия

Upper Triassic‒Middle Jurassic resedimented toe-of-slope and hemipelagic basin deposits in the Dinaridic Ophiolite Belt, Zlatar Mountain, SW Serbia
de
por adulto (o preço varia de acordo com o tamanho do grupo)