Zobrazeno 1 - 10
of 2 131
pro vyhledávání: '"Central Asian Orogenic Belt"'
Publikováno v:
Geoscience Data Journal, Vol 11, Iss 4, Pp 426-432 (2024)
Abstract The Central Asian Orogenic Belt (CAOB) is one of the biggest accretionary orogens in the world. With the development of laser ablation‐inductively coupled plasma‐mass spectrometry (LA‐ICP‐MS), large data of detrital zircon U–Pb and
Externí odkaz:
https://doaj.org/article/afe0908cd8614d93ab65ea62c3930011
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
IntroductionArc-continent collision contributes to the accretion of continental crust in the Central Asian Orogenic Belt. The Chegendalai ophiolitic mélange, located between the Bainaimiao arc and the North China Craton, is important to understandin
Externí odkaz:
https://doaj.org/article/fd96aebb4b824b9692482a23246676bb
Autor:
Xiao‐Miao Tan, Jian‐Bo Zhou, Hui‐Lin Li, Hai‐Yan Wang, He‐Sheng Hou, Wen‐Hui Li, Ying Rao, Rui Gao
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 16, Pp n/a-n/a (2024)
Abstract The Central Asian Orogenic Belt (CAOB) was formed by the aggregation and collage of numerous Paleozoic subduction‐accretion assemblages and Precambrian microcontinental blocks. However, the tectonic nature of the southeastern CAOB remains
Externí odkaz:
https://doaj.org/article/1c2eb165b0874a7bae0cd913dcfe0be2
Autor:
Wang Erteng, Zhai Xinwei, Huang Yaoshen, Li Chengze, Su Ruihuan, Wu Lei, Song Gaorui, Guo Zhiang, Chen Wanfeng, Wang Jinrong
Publikováno v:
Open Geosciences, Vol 16, Iss 1, Pp 1-13 (2024)
Late Paleozoic plutons are widely distributed in the Alxa region, southernmost Central Asian Orogenic Belt, and provided an important clue in constraint for the closing time of the Paleo-Asian Ocean (PAO). In this article, we present new zircon U-Pb
Externí odkaz:
https://doaj.org/article/ddc9b39a7b454cd188c4cfdb0de0c7cd
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 6, Pp n/a-n/a (2024)
Abstract Copper and iron isotopic signatures in sulfide and silicate minerals are important genetic indicators in magmatic sulfide deposits. Kalatongke is a large‐scale magmatic Cu‐Ni sulfide deposit in the Central Asian Orogenic Belt, and one th
Externí odkaz:
https://doaj.org/article/03a85492dfb44c0e924325e1233f190b
Publikováno v:
Руды и металлы, Iss 4, Pp 52-73 (2023)
Regional-scale localization conditions of the Kyzyk-Chadr molybdenum-copper porphyry ore field in the southern folded frame of the Siberian Platform are considered. The porphyry mineralization of the field formed at the Salairian (Early Caledonian) p
Externí odkaz:
https://doaj.org/article/ceac4090a3a346429056420fed7f66b0
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
Externí odkaz:
https://doaj.org/article/8077831bbcfe4d01a6bde95cdd710653
Publikováno v:
Heliyon, Vol 10, Iss 4, Pp e26053- (2024)
The Late Devonian magmatism of the Dananhu arc belt in the Central Asian Orogenic Belt provides a critical geological record. This study provides new comprehensive geochronological, geochemical, and Sr–Nd isotopic data of granodioritic and dioritic
Externí odkaz:
https://doaj.org/article/6454b54d091749cd9a33804a3ce5e7b1
Publikováno v:
Dizhi lixue xuebao, Vol 29, Iss 2, Pp 155-173 (2023)
The eastern Junggar has experienced multistage intra-continental deformations since the late Paleozoic. The checkerboard structure is one of the most notable features of the Junggar Basin, especially the eastern Junggar Basin, and its formation and e
Externí odkaz:
https://doaj.org/article/8ccc1805de6644a4a672c4016f813385
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 6 (2023)
The article presents new data on the age and isotopic (Sr, Nd) characteristics of the Yuzhnoe and Ulan-Ude REE-fluorite occurrences, paragenetically related to alkaline carbonatite magmatism. Age estimates of the fluorite-containing rocks were obtain
Externí odkaz:
https://doaj.org/article/d361e1de829a481b803a52adc320cb69