| [1] |
白文吉,李行.1993.内蒙古贺根山蛇绿岩型铬铁矿中固体包裹体矿物化学成分研究[J].矿物学报,13(3):204-213.
Google Scholar
|
| [2] |
党智财,李俊建,张彤,等.2023.华北地区铬铁矿资源概况及其资源潜力[J].华北地质,46(1):27-32.
Google Scholar
|
| [3] |
黄波,付冬,李树才,等.2016.内蒙古贺根山蛇绿岩形成时代及构造启示[J].岩石学报,32(01):158-176.
Google Scholar
|
| [4] |
李锦轶,高立明,孙桂华,等.2007.内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J].岩石学报,23(3):565-582.
Google Scholar
|
| [5] |
孙立新,张云,李艳锋,等.2020.内蒙古阿巴嘎旗中元古代片麻状花岗岩锆石U-Pb 年龄、地球化学特征及大地构造意义[J].岩石学报,36(03):781-798.
Google Scholar
|
| [6] |
滕学建,付超,李俊建,等.2024.中蒙边境地区主要蛇绿岩带特征及地质意义[J].华北地质,47(3):1-13.
Google Scholar
|
| [7] |
王成,任利民,张晓军,等.2019.内蒙古崇根山蛇绿岩中铬铁矿特征及其构造意义[J].吉林大学学报:地球科学版,49(6):13.
Google Scholar
|
| [8] |
王成,任利民,张晓军,等. 2018.内蒙古贺根山蛇绿岩中铬铁矿特征及大地构造环境[J]. 矿物岩石地球化学通报,37(1):146-155.
Google Scholar
|
| [9] |
Arai S, Miura M. 2016. Formation and modification of chromitites in the mantle[J].Lithos, 264:277-295.
Google Scholar
|
| [10] |
Guo F, Fan W, Gao X, et al. 2010. Sr-Nd-Pb isotope mapping of Mesozoic igneous rocks in NE China: Constraints on tectonic framework and Phanerozoic crustal growth[J]. Lithos, 120(3):563-578.
Google Scholar
|
| [11] |
He Y, Zhu X, She Y, et al. 2021.Mechanism of formation of podiform chromitite: Insights from the oxidation states of podiform chromitites and host peridotites from the Luobusa ophiolite, southern Xizang[J].Ore Geology Reviews, 139:104483.
Google Scholar
|
| [12] |
Miao L, Fan W, Liu D, et al. 2008. Geochronology and geochemistry of the Hegenshan ophiolitic complex: Implications for latestage tectonic evolution of the Inner Mongolia-Daxinganling Orogenic Belt, China[J]. Journal of Asian Earth Sciences, 32(5):348-370.
Google Scholar
|
| [13] |
Xiao W, Windley B, Hao J, et al. 2003.Accretion leading to collision and the Permian Solonker suture, Inner Mongolia, China: Termination of the Central Asian Orogenic Belt[J]. Tectonics, 22(6).1069-1090.
Google Scholar
|
| [14] |
Yang J, Dilek Y, Robinson P T. 2014.Diamonds in Ophiolites:A little-Known Diamond Occurrence[C].
Google Scholar
|
| [15] |
Zhou M, Robinson P T, Su B, et al.2014.Compositions of chromite, associated minerals, and parental magmas of podiform chromite deposits: The role of slab contamination of asthenospheric melts in suprasubduction zone environments[J].Gondwana Research, 26(1):262-283.
Google Scholar
|