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1、岩浆岩成因
2、大陆地壳组成与演化
3、华北克拉通破坏、燕山运动与陆生生物群演化
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- Ai, L., Ping, X., Zheng, J., Su, Y., Ma, Q., Wang, X., 2021. Paleoproterozoic (1.96–1.86？Ga) granites in Xinyang record zoned deep crustal structure and multi-stage reworking beneath the southern North China Craton. Precambrian Research 355, 106079
- 马强, 郑建平, 2009. 辽西北票蓝旗组火山岩锆石U-Pb年龄和Hf同位素组成. 岩石学报 25(12), 3287-3297
- 林向洋, 苏玉平, 郑建平, 马强, 张明民, 2011. 准噶尔盆地克拉美丽气田复杂火山岩储层特征及控制因素. 地质科技情报 30(6), 28-37
- Su, Y., Zheng, J., Griffin, W.L., Zhao, J., Tang, H., Ma, Q., Lin, X., 2012. Geochemistry and geochronology of Carboniferous volcanic rocks in the eastern Junggar terrane, NW China: Implication for a tectonic transition. Gondwana Research 22(3–4), 1009-1029
- Zheng, J.P., Griffin, W.L., Ma, Q., O'Reilly, S.Y., Xiong, Q., Tang, H.Y., Zhao, J.H., Yu, C.M., Su, Y.P., 2012. Accretion and reworking beneath the North China Craton. Lithos 149, 61-78