Citation: | ZHOU Guowu, LIN Min, QIU Guochun, WANG Feng. The redefinition of Xinmin Formation in Zhamuqin area of Horqin Right Wing Middle Banner of Inner Mongolia and its geological significance[J]. Geological Bulletin of China, 2018, 37(9): 1579-1587. |
The Xinmin Formation in Zhamuqin area of Horqin Right Wing Middle Banner of Inner Mongolia were redefined by Inner Mongolia 1:50000 regional survey of four sheets such as Guonaotewula. According to lithologic combination, Xinmin Formation is divided into two lithogic sections:intermediate-acid pyroclastic rock is dominated by a small amount of pyroclastic rocks formed in lower segment overlying Linxi Formation with angular unconformity, whereas the upper part is a thick and thin clastic assemblage, which contains Pinuspollenites, Abiespollenites, Perinopollenites and some other Early-Middle Jurassic micropaleontologic fossils, with no top observed. LA-ICP-MS zircon U-Pb ages are 162.1±1.3Ma and 154.4±2.3Ma, suggesting Middle Jurassic.
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Traffic location of the study area
Geological map of the study area
Sketch showing lower member of Xinmin Formation overlying Linxi Formation with angular unconformity in southeast Taolaoyan
Surveyed geological cross section of Middle Jurassic Xinmin Formation in Taolaoyan
Classification(a), sillicon-alkali relationship(b) and alkalinity diagrams of rocks(c)
AFM(a), An-Ab'-Or(b) and SiO2-K2O(c) diagrams
The frequency curves of volcanic rocks in Washingtion
Primitive mantle-normalized incompatible element spidergram
Chondrite-normalized REE patterns
Zircon CL images of Xinmin Formation (PM301-58)
Zircon U-Pb diagram of PM301-5
Zircon CL images of Xinmin Formation (PM301-104)
Zircon U-Pb diagram of PM301-104