Determination and geological significance of the eclogites from the northern Dabie Mountains, central China

1998 ◽  
Vol 43 (3) ◽  
pp. 253-256 ◽  
Author(s):  
Chunjing Wei ◽  
Zhengang Shan ◽  
Lifei Zhang ◽  
Shiguang Wang ◽  
Zongguang Chang
Keyword(s):  
Central China ◽  
Dabie Mountains ◽  
Geological Significance

Isotopic composition of helium in eclogite from the Dabie Mountains, central China and its geological significance

1998 ◽  
Vol 43 (16) ◽  
pp. 1362-1366 ◽  
Author(s):  
Jianguo Du ◽  
Jianzhen Zhang ◽  
Mingliang Sun ◽  
Youlian Zhang
Keyword(s):  
Isotopic Composition ◽  
Central China ◽  
Dabie Mountains ◽  
Geological Significance

A high precision U–Pb age of metamorphic rutile in coesite-bearing eclogite from the Dabie Mountains in central China: a new constraint on the cooling history

2003 ◽  
Vol 200 (3-4) ◽  
pp. 255-265 ◽  
Author(s):  
Qiuli Li ◽  
Shuguang Li ◽  
Yong-Fei Zheng ◽  
Huimin Li ◽  
Hans Joachim Massonne ◽  
...  
Keyword(s):  
High Precision ◽  
Central China ◽  
Dabie Mountains ◽  
Cooling History

Recycling of deeply subducted continental crust in the Dabie Mountains, central China

Lithos ◽  
2007 ◽  
Vol 96 (1-2) ◽  
pp. 151-169 ◽  
Author(s):  
Fang Huang ◽  
Shuguang Li ◽  
Feng Dong ◽  
Qiuli Li ◽  
Fukun Chen ◽  
...  
Keyword(s):  
Continental Crust ◽  
Central China ◽  
Dabie Mountains

Interaction between subducted continental crust and the mantle — evidences from dabie mountains, Central China

1998 ◽  
Vol 43 (S1) ◽  
pp. 75-75
Author(s):  
S. Li ◽  
Y. Nie ◽  
D. Liu ◽  
S. R. Hart ◽  
Z. Zhang ◽  
...  
Keyword(s):  
Continental Crust ◽  
Central China ◽  
Dabie Mountains

Geochronology, geochemistry, and Hf isotopes of the Jiudinggou molybdenum deposit, Central China, and their geological significance

2015 ◽  
Vol 49 (4) ◽  
pp. 321-342 ◽  
Author(s):  
Yunhui Zhang ◽  
Shouting Zhang ◽  
Mo Xu ◽  
Xingkui Jiang ◽  
Junjun Li ◽  
...  
Keyword(s):  
Central China ◽  
Hf Isotopes ◽  
Geological Significance ◽  
Molybdenum Deposit

Magnetic characteristics of Guangshan loess from northern piedmont of Dabie Mountains, east-central China

2020 ◽  
Vol 222 (2) ◽  
pp. 1213-1223
Author(s):  
Yan Han ◽  
Xiuming Liu ◽  
Guoyong Zhao ◽  
Zhenke Zhang ◽  
Bin Lü ◽  
...  
Keyword(s):  
Loess Plateau ◽  
Southern China ◽  
Central China ◽  
Chinese Loess Plateau ◽  
Magnetic Characteristics ◽  
Dabie Mountains ◽  
Chinese Loess ◽  
Red Soils ◽  
Ferrimagnetic Minerals ◽  
The Chinese Loess Plateau

SUMMARY The loess from the northern piedmont of the Dabie Mountains is in a transition area between loess from the Chinese Loess Plateau, the Quaternary red soils of southern China and the Xiashu loess. Despite its significant location, the study has been inadequate. In this study, the Guangshan section in the northern piedmont of the Dabie Mountains was selected for investigation. Environmental magnetism, geochemistry, colour reflectance and optical diffuse reflection spectroscopy analyses were applied to detect the magnetic variations in the loess. The results showed that (1) the magnetic minerals consisted mainly of magnetite, maghemite, hematite and goethite, which are the same as those in the Quaternary loess from the Chinese Loess Plateau, the Xiashu loess and the Quaternary red soils of southern China. The average magnetic particles were in the pseudo-single domain, like those of the Chinese Loess Plateau loess. (2) Unit III of the Guangshan section (2.4–4 m), with high chemical index of alteration and low Ba-index, was demonstrated as the most strongly developed palaeosol in the whole section, in agreement with field observations (more Fe-Mn films and weakly vermiculated development). However, it exhibited minimal susceptibility values and the lowest concentration of fine ferrimagnetic minerals. Simultaneously, the unit had low hematite to goethite ratio (Hm/Gt), suggesting that the pedogenic environment was humid; and it also had high values of b* and Gt%, implying that there was more goethite. Therefore, we can conclude that excessive soil moisture and intensive pedogenesis dissolved the fine ferrimagnetic minerals originally produced by pedogenesis and transformed them into goethite. These results could help to trace the palaeoclimatic evolution of the study area and clarify the magnetic variations of loess in different climates throughout China.

Field occurrences and petrology of eclogites from the Dabie Mountains, Anhui, central China

Lithos ◽  
1990 ◽  
Vol 25 (1-3) ◽  
pp. 119-131 ◽  
Author(s):  
X. Wang ◽  
Y. Jing ◽  
J.G. Liou ◽  
G. Pan ◽  
W. Liang ◽  
...  
Keyword(s):  
Central China ◽  
Dabie Mountains

scholarly journals Spatio-temporal responses of male Reeves's pheasants Syrmaticus reevesii to forest edges in the Dabie Mountains, central China

2011 ◽  
Vol 17 (1) ◽  
pp. 16-24 ◽  
Author(s):  
Ji-Liang Xu ◽  
Zheng-Wang Zhang ◽  
Yong Wang ◽  
John W. Connelly
Keyword(s):  
Central China ◽  
Dabie Mountains ◽  
Forest Edges ◽  
Spatio Temporal ◽  
Syrmaticus Reevesii
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