RELATIONSHIP OF RUNOFF AND SEDIMENT PRODUCTION BETWEEN HILLSLOPE AND GULLY SLOPE IN A SMALL BASIN IN THE HILLY LOESS REGION, NORTH CHINA

2013 ◽  
Author(s):  
CAI Qiangguo
Keyword(s):  
North China ◽  
Sediment Production ◽  
Loess Region ◽  
Relationship Of ◽  
Hilly Loess Region ◽  
Small Basin

Topographic zonation of infiltration in the hilly loess region, north china

1995 ◽  
Vol 9 (2) ◽  
pp. 227-235 ◽  
Author(s):  
Gang Li ◽  
Shiu Hung Luk ◽  
Qiang Guo Cai
Keyword(s):  
North China ◽  
Loess Region ◽  
Hilly Loess Region

Soft-riser bench terrace design for the hilly loess region of Shaanxi Province, China

2007 ◽  
Vol 80 (1-2) ◽  
pp. 184-191 ◽  
Author(s):  
Shixiong Cao ◽  
Li Chen ◽  
Qi Feng ◽  
Zhande Liu
Keyword(s):  
Shaanxi Province ◽  
Loess Region ◽  
Hilly Loess Region

scholarly journals RELATIONSHIP OF THE FORMATION OF OROGENS AND SEDIMENTARY BASINS OF ASIA IN THE MESOZOIC-CENOZOIC

2021 ◽  
Vol 2 (1) ◽  
pp. 25-31
Author(s):  
Mikhail M. Buslov ◽  
Anna V. Kulikova
Keyword(s):  
North China ◽  
Sedimentary Basin ◽  
Sedimentary Basins ◽  
Asian Continent ◽  
Active Margin ◽  
Mountain Systems ◽  
Orogenic Belts ◽  
Relationship Of

The stages of the formation of mountain systems (orogens) and sedimentary basins of Asia are highlighted and an analogy is given. The stages are manifested in the Jurassic, Cretaceous, and Cenozoic as a result of collisions to the southern active margin of the Asian continent, respectively, of the Quingtang, North China, and Indian continental blocks, which led to the formation of large intracontinental orogenic belts that are the source of sedimentary basin demolition.

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