桂林工学院学报
桂林工學院學報
계림공학원학보
JOURNAL OF GUILIN INSTITUTE OF TECHNOLOGY
2009年
2期
169-182
,共14页
剪切带%递进变形%成矿机理%显微构造%压溶作用%缝合线%金山金矿
剪切帶%遞進變形%成礦機理%顯微構造%壓溶作用%縫閤線%金山金礦
전절대%체진변형%성광궤리%현미구조%압용작용%봉합선%금산금광
shear zone%progressive deformation%mineralization mechanism%microscopic structure%pressure solution%stylolite%Jinshan gold deposit
在对江西金山金矿控矿韧性剪切带内岩石和矿石的显微构造分析基础上,对剪切带的递进变形与成矿机理进行探讨.研究发现,金山韧性剪切带在韧性-韧脆性递进剪切变形过程中发育3类石英脉透镜体或石香肠构造;剪切压溶和缝合线构造在金山韧性剪切带内强烈发育;扩散蠕变机制是金山韧性剪切带重要的变形机制.大量缝合线构造的形成增强了岩石的孔隙度和渗透率,有利于流体的迁移和沉淀.金山剪切带内变形和成矿作用经历了漫长复杂的地质过程,粗略估算至少跨过了72 Ma.在递进剪切变形过程中经历多种构造变形机制,如经历了以透入性片理为代表的韧性剪切变形机制到以"次级剪切面"构造网络为代表的韧-脆性剪切变形机制的转换.剪切带的递进剪切变形自始至终控制着金的成矿作用过程,没有递进剪切变形也就没有金山金矿的形成.
在對江西金山金礦控礦韌性剪切帶內巖石和礦石的顯微構造分析基礎上,對剪切帶的遞進變形與成礦機理進行探討.研究髮現,金山韌性剪切帶在韌性-韌脆性遞進剪切變形過程中髮育3類石英脈透鏡體或石香腸構造;剪切壓溶和縫閤線構造在金山韌性剪切帶內彊烈髮育;擴散蠕變機製是金山韌性剪切帶重要的變形機製.大量縫閤線構造的形成增彊瞭巖石的孔隙度和滲透率,有利于流體的遷移和沉澱.金山剪切帶內變形和成礦作用經歷瞭漫長複雜的地質過程,粗略估算至少跨過瞭72 Ma.在遞進剪切變形過程中經歷多種構造變形機製,如經歷瞭以透入性片理為代錶的韌性剪切變形機製到以"次級剪切麵"構造網絡為代錶的韌-脆性剪切變形機製的轉換.剪切帶的遞進剪切變形自始至終控製著金的成礦作用過程,沒有遞進剪切變形也就沒有金山金礦的形成.
재대강서금산금광공광인성전절대내암석화광석적현미구조분석기출상,대전절대적체진변형여성광궤리진행탐토.연구발현,금산인성전절대재인성-인취성체진전절변형과정중발육3류석영맥투경체혹석향장구조;전절압용화봉합선구조재금산인성전절대내강렬발육;확산연변궤제시금산인성전절대중요적변형궤제.대량봉합선구조적형성증강료암석적공극도화삼투솔,유리우류체적천이화침정.금산전절대내변형화성광작용경력료만장복잡적지질과정,조략고산지소과과료72 Ma.재체진전절변형과정중경력다충구조변형궤제,여경력료이투입성편리위대표적인성전절변형궤제도이"차급전절면"구조망락위대표적인-취성전절변형궤제적전환.전절대적체진전절변형자시지종공제착금적성광작용과정,몰유체진전절변형야취몰유금산금광적형성.
Microscopic deformation structures observed in deformed rocks and ores from Jinshan auriferous ductile shear zone of Jinshan gold deposit,Jiangxi Province,are examined and analyzed.Gold mineralization process during progressive shear deformation in the ductile shear zone is discussed.Three classes of quartz-vein boudinage are found developed within the ductile shear zone with respect to vein and boudinage characteristics and timing of major-phase mineralization.The discovery covers intensive pressure solution and pressure dissolution structures of stylolites or dissolution seams developed in the ductile shear zone in detail.The extensively and intensively developed stylolites help enhance porosity and permeability of the shear zone rocks,and provide pathways for migration of fluids as well as space for silica precipitation.Their presence indicates that fluids-enhanced diffusion creep or diffusional mass transfer is not only an important deformation mechanism but also a critical component of mineralization mechanism for Jinshan auriferous ductile shear zone.The paper estimates a minimum 72 million years span for the progressive deformation and mineralization process associated with multiple deformation mechanisms,and underwent a significant deformation regime transfer from penetrative schistosity-dominated fabric of ductile deformation to a non-penetrative (at outcrop and microscopic scales) network of "second-order" shear structures of ductile-brittle deformation.It is concluded that the mineralization process was caused by the progressive shear,and that there would be no such a large gold deposit without the prolonged progressive deformation.