dong Alufudong - 阿卢古洞

ZHANG, Shouyue (1993): Speleotour in China.-

Proceedings XI Intern. Congress of Speleology, 2nd-8th August 1993, Beijing 1993: 215-216 (3 tab.) (chines. summ.).

Data on additional 33 well exploited show caves are presented. There are over 200 show caves in China, including 41 major show caves as of 1986 (see: Communications 9th Intern. Congress of Speleology Vol.2: 225-228). (RB).
Source : BBS
BALAZS, Dénes (1990): A dél - Kinai - karszvidék föbb barlangtípusai (Main cave types in the south chinese karst region).-

Karszt és Barlang I/90 :53-60 (hungar.; engl.summ.) (5fig.,phot.)

Caves in China are systematized on the basis of orographic position and dimensions of the karstic block as well as the origin of the cave. (1) caves of the fenglin (peak forest) (footcaves, fossil remnants); (2) caves of the fengcong (peak cluster) (dolines, avens, stream caves due to allogenic water - course); (3) caves of the highland fenglin and fengcong (Guizhou type) (mostly young vadose caves); (4) caves of the karst plateaux (Guanxi or Guilin type) (mostly active or dry fluvial caves). (RB)
Source : BBS
DUSAR, M.; ZHANG, Shouye (1991) : "East Yunan 1991". Geological and speleological reconnaissance of the East Yunan Karst (PR China). Preliminary results of a field trip between 17.12.1990 and 3.01.1991.-

Professional Paper (Service Géologique de Belgique), 1991/4, no248 (RV)

Source : BBS

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Sources et analyses : BBS, GKC, IGU KC