The origin of bedding-parallel fibrous calcite veins in the Lower Permian Chihsia Formation in western Hubei Province, South China

2015 ◽  
Vol 60 (20) ◽  
pp. 1778-1786
Author(s):  
Hao Yu ◽  
XiQiang Zhou ◽  
JianGuo Wang ◽  
Chuan Guo ◽  
HengYe Wei ◽  
...  
2019 ◽  
Vol 62 (10) ◽  
pp. 1645-1658 ◽  
Author(s):  
Qiangfen Ma ◽  
Qinglai Feng ◽  
Wenchao Cao ◽  
Lei Zhang ◽  
Yan Ye ◽  
...  

2019 ◽  
Vol 109 ◽  
pp. 381-393 ◽  
Author(s):  
Yiquan Ma ◽  
Yongchao Lu ◽  
Xiaofeng Liu ◽  
Gangyi Zhai ◽  
Yufang Wang ◽  
...  

2019 ◽  
Vol 30 (5) ◽  
pp. 1059-1074 ◽  
Author(s):  
Bo Yang ◽  
Hanxiao Li ◽  
Paul B. Wignall ◽  
Haishui Jiang ◽  
Zhijun Niu ◽  
...  

2019 ◽  
Vol 320 ◽  
pp. 232-252 ◽  
Author(s):  
Zhongwu Lan ◽  
Yuji Sano ◽  
Takuya Yahagi ◽  
Kentaro Tanaka ◽  
Kotaro Shirai ◽  
...  

2006 ◽  
Vol 43 (2) ◽  
pp. 121-133 ◽  
Author(s):  
Mutwakil Nafi ◽  
Xia Wenchen ◽  
Zhang Ning

Four neogondolellid conodont interval zones were recognized across the Changhsingian stage at Ganxi section, western Hubei Province, south China. They are in ascending order: the Clarkina wangi Zone, the Clarkina changxingensis changxingensis Zone, the Clarkina changxingensis yini Zone, and the Clarkina meishanensis meishanensis Zone. The present study suggests that the base of the Changhsingian can be defined by the first appearance datum (FAD) of Clarkina wangi within an evolutionary lineage from Clarkina longicuspidata to Clarkina wangi. The Wuchiapingian–Changhsingian boundary can be placed at the base of bed 104 at Ganxi section, south China because of the first occurrence of Clarkina wangi.


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