Based on the organic geochemical studies on two typical Carlin-type deposit
s in southwestern Gulzhou, as well as the comparison between the two deposi
ts in terms of geological background, igneous rock, paleo-oilfield, lithofa
cies and paleogeographical and geochemical features, two kinds of Carlin-ty
pe deposit were proposed: Lannigou Type and Getang Type. The former include
s Lannigou, Banqi and Yata gold deposits. These deposits are hosted by turb
idite, geographically situated in the southwest of the mineralized district
, and related genetically to paleo-oilfields. The latter includes Getang, Z
imudang and Dachang gold (mercury and thallium) deposits, situated geograph
ically in the northwest of the mineralized district where Emishan basalt co
mmonly occurs. These deposits are associated with reduction of coaly organi
c matter.