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朱光

(合肥工業大學教授)

鎖定
朱光,男,1959年出生,合肥工業大學教授。代表作品有《Journal of Structural Geology》等。 [1] 
中文名
朱光
外文名
Guang Zhu
國    籍
中國
民    族
出生日期
1959年3月11日
畢業院校
英國威爾士大學
職    業
教師
主要成就
一九九五年機械工業部科技進步一等獎
出生地
合肥
代表作品
《Journal of Structural Geology》
所屬系所
資源與環境工程學院

朱光人物經歷

合肥工業大學地質學教授、博士導師。中國地質學會構造地質與地球動力學專業委員會常委。國家百千百萬人才工程國家級人選,中國地質學會構造地質與地球動力學專業委員會常委,國家自然科學基金委員會地球科學部專家評審組成員,《地質科學》與《地質學報》編委。 [1] 

朱光研究方向

主要研究方向:
1.中國東部斷裂構造與動力學
2.構造同位素年代學
3.盆地動力學與油氣 [1] 

朱光主要貢獻

主持的在研項目
1.國家自然科學基金重點項目(2019--2023):“郯廬斷裂帶起源機制研究”(編號:41830213)
2.國家重點研究發計劃深地項目二級課題(2016-2020):,“華北東部中生代構造演化與控礦機制”
(編號:2016YFC0600102) [1] 

朱光主要論著

代表性論文:
[1] Xu, J W., Zhu, G., Tong, W. X., Cui, K. R. & Liu, Q.1987.Formation and evolution of the Tancheng-Lujiang wrench fault system: a major shear system to the northern of the Pacific Ocean. Tectonophysics, 134: 273-310.
[2] Zhu, G. 1993. Structural and deformation characteristics of the southern segment of the Tianmushan-Baijishan major shear zone. In: The Tancheng-Lujiang Wrench Fault System (Edited by XU Jiawei), 177-183. John Wiley & Sons Ltd, UK.
[3] Zhu, G., Xu, J. W., Gao, D. L., Lin, S. F. & Ma,G.F.1993. Structural characteristics and deformation of the Changle-Nanao megashear zone along the Southeast China coast. In: The Tancheng-Lujiang Wrench Fault System (Edited by XU Jiawei), 201-209. John Wiley & Sons Ltd, UK.
[4] Zhu, G. and Xu, J. W. 1994. Isotopic constraints on the Palaeozoic evolution of the Shandong Peninsula, N.E. China. Journal of Southeast Asian Earth Sciences, 9 (3): 241-248.
[5] Xu, J. W. and Zhu, G., 1994. Tectonic models of the Tan-Lu fault zone, eastern China. International Geology Review, 36: 771-784.
[6] Zhu G., Xu J. W. & Liu G. S. 1999. Tectonic Pattern and dynamic mechanism of foreland deformation in the Lower Yangtze region. Gondwana Research, 2(4): 557-559.
[7] 朱光,宋傳中,王道軒,劉國生,徐嘉煒.2001.郯廬斷裂帶走滑時代的Ar/Ar年代學研究及其構造意義.中國科學(D輯),31(3):250-256
[8] 朱光,劉國生,W J Dunlap, C Teyssier,王勇生,牛漫蘭.郯廬斷裂帶同造山走滑運動的Ar/Ar年代學證據.科學通報, 2004, 49(2):190-198.
[9] Zhu, G., Wang, Y.S., Liu, G. S., Niu, M. L., Xie, C. L., Li, C. C. 2005. Ar/Ar dating of strike-slip motion on the Tan-Lu fault zone, East China.Journal of Structural Geology, 27(8): 1379-1398.
[10] 朱光,謝成龍,王勇生,牛漫蘭,劉國生. 郯廬高壓走滑韌性剪切帶特徵及其Ar/Ar定年.岩石學報,2005,21(6):1687-1702
[11]Zhu, G., Liu,G. S., Niu, M. L., Xie, C. L., Wang, Y. S. , Xiang, B. W., 2009. Syn-collisional transform faulting of the Tan-Lu fault zone, East China. International Journal of Earth Sciences, 98(1):135-155
[12] Zhu, G., Niu, M. L., Xie, C. L., Wang, Y. S.2010. Sinistral to normal faulting along the Tan-Lu Fault Zone: evidence for geodynamic switching of the East China continental margin. Journal of Geology, 118(3): 277-293.
[13] Zhu, G., Xie, C. L., Chen, W., Xiang, B. W., and Hu, Z. Q. 2010. Evolution of the Hongzhen metamorphic core complex: evidence for Early Cretaceous extension in the eastern Yangtze craton, eastern China. Geological Society of America Bulletin, 122: 506-516
[14] Zhu, G., Jiang, D.Z., Zhang, B. L., Chen, Y. 2012. Destruction of the eastern North China Craton in a backarc setting: evidence from crustal deformation kinematics. Gondwana Research, 22:86-103.
[15]Zhang, B., Zhu, G*., Jiang,D., Li,C., Chen, Y. 2012. Evolution of the Yiwulushan metamorphic core complex from distributed to localized deformation and its tectonic implications, Tectonics, 31, TC4018,
[16]林少澤,朱光,嚴樂佳,宋利宏,劉備。2013.燕山構造帶晚古生代擠壓變形事件的構造與年代學證據。科學通報,58(34):3597-3609
[17]嚴樂佳, 朱光, 林少澤, 趙田.2014. 沂沭斷裂帶新構造活動規律與機制. 中國科學(地球科學),44(7): 1452-1467.
[18]林少澤, 朱光, 趙田, 宋利宏, 劉備.2014. 燕山地區喀喇沁變質核雜巖的構造特徵與發育機制.科學通報,59(32):3174-3189.
[18]趙田, 朱光, 林少澤, 嚴樂佳, 姜芹芹.2014. 郯廬斷裂帶張八嶺隆起段變質岩的原巖時代與變形機制. 中國科學(地球科學),44(10): 2112-2129.
[19]Zhu, G., Chen, Y., Jiang, D. Z., Lin, S. Z. 2015.Rapid change from compression to extension in the North China Craton during the Early Cretaceous: Evidence from the Yunmengshan metamorphic core complex. Tectonophysics, 656: 91-110.
[20]Zhu, G., Hu, W., Song, L. H., Liu, B. 2015. Quaternary activity along the Tan-Lu fault zone in the Bohai Bay, East China: Evidence from seismic profiles. Journal of Asian Earth Sciences, 114 (Part 1):5-17.
[21] Liu, B., Zhu, G*., Zhai, M. J., Gu, C. C., Liu, S. 2015. Quaternary faulting of the Jiangsu part of the Tan-Lu Fault Zone, East China: Evidence from field investigations and OSL dating. Journal of Asian Earth Sciences, 114 (Part 1): 89-102.
[22]Zhao, T., Zhu, G*., Lin, S. Z., Wang, H.Q. 2016. Indentation-induced tearing of a subducting continent: Evidence from the Tan–Lu Fault Zone, East China. Earth-Science Reviews, 152: 14-36.
[23]顧承串,朱光,翟明見,林少澤,宋利宏,劉備.2016. 依蘭-伊通斷裂帶中生代走滑構造特徵與起源時代. 中國科學: 地球科學 46(12): 1579-1601.
[24]Zhu, G., Wang, Y. S., Wang, W., Zhang, S., Liu, C., Gu, C. C., Li, Y. J. 2017. An accreted micro-continent in the north of the Dabie Orogen, East China: Evidence from detrital zircon dating. Tectonophysics, 698: 47-64.
[25]Gu, C. C., Zhu, G*.,Zhang, S., Liu, C., Li, Y. J., Lin, S. Z., Wang, W.2017. Cenozoic evolution of the Yilan-Yitong Graben in NE China: An example of graben formation controlled by pre-existing structures. Journal of Asian Earth Sciences, 146:168-184.
[26]張帥,朱光,顧承串,劉程,李雲劍,趙田,王薇.2017.遼-吉造山帶東南邊界位置探討.科學通報,62(24):2814-2828.
[28]Liu, C., Zhu, G*., Zhang, S., Gu, C. C., Li, Y. J., Su, N., Xiao, S. Y. 2018. Mesozoic strike-slip movement of the Dunhua–Mishan Fault Zone in NE China: A response to oceanic plate subduction. Tectonophysics, 723: 201–222.
[29]朱光,劉程,顧承串,張帥,李雲劍,蘇楠,肖世椰.2018.郯廬斷裂帶晚中生代演化對西太平洋俯衝歷史的指示.中國科學: 地球科學,48(4): 415-435.
[30] Gu, C. C., Zhu, G*., Li, Y. J., Su, N., Xiao, S. Y., Zhang, S., Liu, C. 2018. Timing of deformation and location of the eastern Liaoyuan Terrane, NE China: Constraints on the final closure time of the Paleo-Asian Ocean. Gondwana Research, 60: 195-212.
[31] Zhang, S., Zhu, G*., Liu, C., Li, Y., Su, N., Xiao, S., & Gu, C. 2018. Strike-slip motion within the Yalu River Fault Zone, NE Asia: The development of a shear continental margin. Tectonics, 37, 1771-1796.
[32] Li, Y. J., Zhu, G*., Gu, C. C., Su, N., Xiao, S. Y., Zhang, S., Liu, C., Xie, C. L. 2018. Structural evolution of the Paleoproterozoic Trans-North China Orogen: Evidence from the Xiaoqinling region, central China. Precambrian Research, 316: 244-274.
[33] 肖世椰,朱光,張帥,劉程,蘇楠,尹浩,吳曉冬,李雲劍. 2018.遼東五龍金礦區成礦期構造過程與岩脈就位機制. 科學通報 63(28-29): 3022-3036.
[34] Liu, C., Zhu, G*., Xie, C. L., Zhang, S., Li, Y. J., Su, N., Xiao, S. Y. 2019. Location and sinistral displacement of the eastern Liaoyuan Accretionary Belt along the Tan–Lu Fault Zone, NE China. Journal of Asian Earth Sciences, 147, 409-422.
[35] Zhang, S., Zhu, G*., Liu, C., Li, Y., Su, N., Xiao, S. 2019. Episodicity of stress state in an overriding plate: Evidence from the Yalu River Fault Zone, East China. Gondwana Research 71: 150-178.
[36] Hao, W. X., Zhu, G., Zhu, Z. X. 2019.Timing of the Yanshan Movement: evidence from the Jingxi Basin in the Yanshan fold-and-thrust belt, eastern China. International Journal of Earth Sciences, 108:1961–1978.
[37] Su, N., Zhu, G*., Liu, C., Zhang, S., Li, Y. J., Yin, H., Wu, X. D. 2020. Alternation of back-arc extension and compression in an overriding plate: evidence from Cretaceous structures in the western Liaoning region, eastern China. International Journal of Earth Sciences. 109: 707-727.
參考資料
  • 1.    朱 光  .合肥工業大學資源與環境工程學院[引用日期2023-01-04]