1) Hengshan complex
恒山杂岩
1.
show that the climax value of Hengshan complex’s (2520 Ma) is 20Ma less than Wutai complex’s (2540 Ma), which coincides with the opinion of Hengshan complex being the arc root of Wutai arc.
近10年在恒山和五台地区所获得的大量同位素年代学资料,统计发现恒山杂岩的同位素年龄峰值比五台杂岩大致要年轻20Ma,这与恒山-五台地区为岛弧根带-岛弧关系的推论相符合。
2) volcanic complex
火山杂岩
1.
Characteristics of Early Cretaceous volcanic complexes in the Genhe area in the northern segment of the Da Hinggan Mountains:with a discussion of their genesis;
大兴安岭北段根河地区早白垩世火山杂岩特征及成因探讨
3) Long-shan Complex
陇山杂岩
4) Mashan Complex
麻山杂岩
1.
The Mashan Complex: SHRIMP U- Pb zircon evidence for a Late Pan- African metamorphic event in NE China and its implication for global continental reconstructions;
中国东北麻山杂岩晚泛非期变质的锆石SHRIMP年龄证据及全球大陆再造意义
5) Dongshan Complex
东山杂岩
1.
The Early Archaean Geological Evolution of the Dongshan Complex, Anshan Region: Constrained by SHRIMP Geochronology and Nd & Hf Isotopes;
鞍山地区东山杂岩太古宙早期地质演化—SHRIMP年代学及Nd、Hf同位素制约
6) Lianyunshan complex
连云山杂岩
1.
Regional metamorphism of the Lianyunshan complex in the eastern Xuefeng mountain belt and its significance on crust-mantle interaction;
雪峰山东段—连云山杂岩区域变质特征及岩石圈深部作用信息
2.
The Lianyunshan complex, cropping in the Jiuling Mufushan range in the northeastern Hunan Province, belongs to the paleo Proterozoic crystalline basement rocks.
出露于湘东北九岭—幕阜山岭之中的连云山杂岩属于古元古代结晶基底岩系。
3.
GUO Le-qunTANG Xiao-shanPEN He-qiu,,(Hunan Institute of Geology SurveyXiangtan Hunan 411100China)Abstruct: The Lianyunshan complex is metamorphic rock formed for regional metamorphism ofhigh greenschist -amphibolite facies and matization and contact thermal metamorphis.
连云山杂岩是经区域高绿片岩相—角闪岩相变质、混合岩化及热接触变质作用而形成的变质岩系，其变质矿物组合为St+Sill+Cr+Hb+Ab+Bi+Ms+Pl+Qz。
补充资料：杨恒山
杨恒山 杨恒山 明代医家。履贯未详。精于医道，于《伤寒论》颇有研究，尝撰有《伤寒宗陶全生金镜录》一书，未见行世。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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