Bangbu

The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.

Bangbu

 

Bengbu, city and port in eastern China, in An-hwei Province, on the lower course of the Huaihe River at the point at which a railroad line crosses it. Population, 267,000 (1959; estimate). Bangbu is an important trade and transportation center; grains, salt, and coal (from the Huainan mines) are shipped out through it. There is agricultural machine-building, ship repair, and production of metal articles; and food, tobacco, and paper enterprises.

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.
References in periodicals archive ?
The NHMB contains many Sb, Au, Sb-Au, Pb-Zn, and Sb-Pb-Zn-Ag deposits, and the Zhaxikang Sb-Pb-Zn-Ag, the Mazhala Au-Sb, the Chalapu Au, the Bangbu Au, the Shalagang Sb, the Cheqiongzhuobu Sb deposits are representative (Figure 1(b)) [7, 25].
The Fe-Zn Isotopic Characteristics and Fractionation Models: Implications for the Genesis of the Zhaxikang Sb-Pb-Zn-Ag Deposit in Southern Tibet
The first mineralization event is related to multiple seafloor volcanic events during a synsedimentary period (220~130Ma; e.g., the first pulse of mineralization in the Zhaxikang Sb-Pb-Zn-Ag deposit); the second mineralization event is associated with a metamorphic fluid system during the syn-collision period (60~42 Ma) of Indian and Eurasian plates that formed several orogenic Au-Sb deposits (e.g., Nianzha and Bangbu Au deposits); and the third mineralization event relates to the magmatic-hydrothermal activity during the postcollision period (25 Ma to present) and has formed some W-Sn, Pb-Zn (Ag), and Sb-Au deposits (e.g., Dongga W-Sn and Shalagang Sb deposits).
Geology, Mineralogy, Fluid Inclusion, and H-O-S-Pb Isotope Constraints on Ore Genesis of the Keyue Sb-Pb-Zn-Ag Deposit in Southern Tibet
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