Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Guo-Qi He"'
Autor:
Lee Griffiths, Dalai Zhong, Junfeng Gong, Jianqing Ji, Jin-Duo Wang, Qinqin Xu, Guo-Qi He, Lei Zhao, Jing Zhou
Publikováno v:
Earth-Science Reviews. 126:178-205
The Northern Xinjiang region is located in the southwestern part of the Central Asian Orogenic Belt (CAOB, also known as the Altaid Tectonic Collage). Despite extensive research aimed at understanding the crustal growth of the CAOB and the evolution
Publikováno v:
Advanced Materials Research. :1634-1640
Based on the experimental conditions of generation grinding of spiral bevel gear, the grinding orthogonal test design of L16(45) is made, and the results of grinding orthogonal test are obtained. On this basis, the range and variance analyses are car
Publikováno v:
Advanced Materials Research. :1405-1411
According to the theory of heat transfer, it analyzed the calculating method of tooth friction heating in the process of face gear tooth meshing. It emulational analyzes the thermal coupling of the face gear with ANSYS/LS-DYNA, and extracts the state
Publikováno v:
Earth-Science Reviews. 109:74-93
The Tian Shan of Central Asia is located in the southwestern part of the Central Asian Orogenic Belt (CAOB, also known as the Central Asian Orogenic System or CAOS). Formation of the South Tian Shan Orogen is a diachronous, scissors-like process duri
Publikováno v:
Applied Mechanics and Materials. 127:560-568
Through the analyses of experiment,mechanism of dislocation and coupling of grinding temperature and deformation field,many conclusions are gotten.Firstly,a tempering metamorphic layer of lower hardness is formed in hardening zones of grinding layer
Publikováno v:
Lithos. 115:137-152
North Xinjiang, Northwest China, is made up of several Paleozoic orogens. From north to south these are the Chinese Altai, Junggar, and Tian Shan. It is characterized by widespread development of Late Carboniferous–Permian granitoids, which are com
Publikováno v:
Chinese Science Bulletin. 44:1119-1123
In Tuoyun area of southwestern Tianshan, mantle and lower crust xenoliths are present in the volcanic rocks with ages of 101–123 Ma. Mantle xenoliths include mineral megacrysts such as kaersutite and pargasite, feldspar, biotite, and rare pyroxene
Publikováno v:
Science in China Series D: Earth Sciences. 42:113-119
The late Paleozoic postcollisional granitoids, mafic-ultramafic complexes, and volcanic rocks are extensively distributed around the Junggar Basin; they are generally characterized by positive eNd(t) values, implying that the magmas were mantle-deriv
Publikováno v:
Chinese Science Bulletin. 44:380-381