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The main body of Xinglongshan Nature Reserve is from Xinglongshan、Magnatal Mountain and Mountain Valley Composition。The location of the earth's structure belongs to the southeast end of Qin Qi in the Qin Qi band between the Qilian ground m88 live casino gamesslot fold system and the Qinling floor folds，The secondary construction unit is Qingshi Ridge -Ma Tuoshan Folding Dome and Xinglong Mountain Caval with the Horses Mountain horizontal band。Former Zhendan and Zhendanpi，This area accepts a set of floor -shaped sandstones、Pink sandstone、Mud rock、acidic and neutral volcanic debris rock、Middle volcanic rocks and carbonate rocks such as mellow deposits。Lu Liang Movement of the former Zhendan Ji made it fold back，Forms a construct contour of the horseshill mountain backward and the back -to -back，and accompanied by different nature of fracture activities，It produced a strong mixed rockization in the later period，All kinds of hybrid rocks in the Guangbian Mountain District have been formed。Galidong Movement further suffers from regional deterioration in this area，Lile the constructive features of Xinglongshan Duplex and Slip。Relatively speaking，Yanshan Movement and Himalayan movement is not very strong in this area，On the contrary，New structure movement M88 Online Live Casinois more active，Make this area constantly rising。

The exposed floors in the protected area are mainly: the front Zhendan system (anz), Zhendan Department (Z), Jurassic (J), White 垩 (K), the third series (N) and the fourth series (Q）。

1, the former Zhendan is the horse title mountain group (anzmx）

The deepest stratum in the Maibuka Mountain Group Reserve，The rock nature is mainly various types of mixed rocks，Followed by mixed rocky slices hemp、Ship Rock、Long British Change Rock、Corner flash rock and carbonate rock。According to the codes of Huang Aigou, the Mazi Mountain Cluster can be divided into above、Middle、The next three groups。

2, shocked Dan Xinglong Mountain Group (z1xn）

Xinglong Mountain Group is mainly divided into Xinglong Mountain and its surroundings，​​The rock nature is mainly a set of mountain rocks、debris rocks and carbonate rocks，Unconduct contact with the former Zhendan Mountain Group。According to the characteristics of the rock, the Xinglong Mountain Group is divided into four groups，Each m88 reviewgroup is integrated contact relationship。

3, Jurassic (J）

distributed in Shuichagou at the northern foot of Xinglong Mountain、Tieyegou area，In Qinglougou、kiln gap、Gaojiawan has sporadic revealing。According to the composition of rocky and the types of fossils contained, it is divided into lower Jurassic Agan Town group (j1Ag) and Shangjura Tongtonggou Group (j2-3ty）.

4, Baiji Department of Tonghekou Group (K1HK）

Mainly distributed in Ma Tu Tuoshan、Xinglong Mountain Follower。In addition，In Majia Temple、Yangzhai has sporadic revealing。The rock nature is mainly a set of purple -red、Blue -green mud rock、shale、Sandstone mutual layers，Plucking thin layer of gravel rock and mudstone，The bottom is fragrance。Uncondurable contact relationship with the middle and upper Jurassic Terramtae group or the older floors，Part of the part of the part of the section contact relationship。

5, the third series of the Linxia Group (n2l）

less exposed in the third series in the protected area，Only the new Linxia m88 live casino gamesgroup has sporadic revealing in the northwest of Yangzhai。The rock nature is mainly a red sandstone deposited in the lake phase、Calcium Gravite、Mud rocks and mud rocks，Small thickness。False integrated contact relationship with the inferior white crickets in the river。

6, Fourth Series (Q）

The fourth series covers a wide range of coverage，Most of them are distributed on hillside、River Bed and Gully Zone。mainly from loess、Sand and Gravel Earth Composition，Is some wind accumulation、Leap and flood accumulation。The revealing in the protected area is mainly the update unified loess，Most distributed on the front slope of the mountain，Ten composed of gray -yellow loosely loess，Unstable thickness; in addition, a new unified deposit、Hong Ji，Mainly distributed in Xinglong Mountain，Mountain Valley of the Mountain Mountains，It consists of secondary loess and gravel。These formation of rhine bed Ⅰ and level Ⅱ flood、Leaping ground。

      Editor in charge: Wang Yanting