摘要
本文研究了湘中禾青地区中上泥盆统碳酸盐岩的成岩作用及其与成矿的关系。根据野外工作、镜下观察、C、O同位素特征和痕量元素特征的研究,区内碳酸盐岩成岩作用方式主要有压实作用、胶结作用、新生变形和白云岩化作用4种。它们经历了淡水渗流、淡水潜流、海水和埋藏地下混合水4种成岩环境。由于含矿层以上成岩环境的开放性和其下成岩环境的闭塞,埋藏地下混合水成岩作用使矿质富集而形成工业矿体。
On the basis of geology, petrology and geochemistry, the diagenesis of carbonate rocks in the Middle-Upper Devonian series in Heqing district and its relation to the formation of Pb-Zn ore deposit are studied by means of field investigation and various techniques in laboratory in this pater.
In the studied area the outcroped strata are mainly three formation: the Middle Devonian Qiziqiao Formation (D2q), the Upper Dvonian Shetianqiao Formation (D3s) and Xikuangshan Formation (D3x) . According to the differences in lithologic characters, Qiziqiao Formation can be subdivided into three members, Shetianqiao Formation and Xikuangshan Formation both into two members. All of them are mainly composed of limestone with few of terrigenous sedimentary rocks. Sedimentary characteristics show that the Middle-Upper Devonian series may be classified into five microfacies (1) intertidal mud flat (including tidal-flat in clear water and tidal-flat in muddy water), (2) grain beach, (3) bioreef, (4) restricted bulf, (5) subtidal tempestite.
The field investigation, observation under microscope and distribution characteristics of carbon and oxygen stable isotopes and the trace elements show that the Middle- Upper Devonian carbonate rocks have four principal diagentic manners i. e. : compaction, cementation, neomorphism and dolomization. Compacton is one of the most common diagentic manners, causing decrease of porosity and compact of lime. Neomorphism make micrite enlarge into microsparry and pseudosparry, and considered as the second one. The Middle- Upper Devonian carbonate rocks in studied area experienced four diagenetic environments. They are: (1) Vadose zone of freshwater, (2) Phreatic zone of freshwater, (3) Seawater and (4) Burial- underface dorage zone, among which the influnce of burial-underface dorage zone diagenetic environment is the largest to carbonate rocks in the area. The properties of carbon-oxygen stable isotopes and trace elements suggest that the diagenetic environments of bioreef, grain beach, tidal-flat in clear and subtidal tempestite are open relatively and the diagenetic fluid are active and fresh water flow in. But the diagenetic fluid of tidal-flat in muddy water and restricted gulf are stagnant relatively. As the result of the the open diagenetic environment over ore-bearing strata and the stagnant of diagenetic fluid beneath it, burial-underface dorage diagenesis made mineral elements to be enriched into industrial deposit.
出处
《沉积学报》
CAS
CSCD
北大核心
1990年第3期66-74,共9页
Acta Sedimentologica Sinica
基金
国家自然科学基金
