赣东北断裂带铜、金成矿控制因素耦合作用及其模拟实验

赣东北断裂带钢、金成矿受地层、岩性、岩浆活动、构造作用等多种因素的控制，这些控制因素在铜、金成矿过程中起着相互制约、相互影响、相互促进的耦合作用。本文从构造与成矿的密切关系──即从构造地球化学入手，综合研究地层、岩性、岩浆活动、构造作用等控制因素在赣东北断裂带钢、金成矿过程中的相互影响，相互促进的耦合作用，并运用矿床地球化学开放研究实验室的构造化学实验条件，进行构造控矿和铜、金成矿控矿因素之间的相互影响，相互促进耦合作用的模拟实验，获得良好的实验效果。它将为深入研究该带钢金成矿规律，成矿预测提供实验资料和实验依据。

COUPLING IN ORE - CONTROLLING FACTORS OF CU AND AU IN THE NORTHEAST JIANGXI FRACTURE ZONE AND SIMULATING EXPERIMENTS

Cu and An ore deposits in the Northeast Jiangxi fracture zone were controlled by many factorssuch as strata, rocks, magmatic activity and tectonism, etc. These factors were coupled in the ore-forming Process of Cu and An ore deposits, Tectono-geochemical methods were used in this paper tostudy the coupling of ore-controlling factors such as strata, rocks, magmatic activity and tectonism inthe Cu and An ore-forming process in the Northeast Jiangxi fracture zone. Experimental apparatusof the Tectono-Geochemical Laboratory was fully utilized to simulate the coupling of tectonic-controlled metallogenesis and Cu and An ore-controlling factors, and better experimental resultswere obtained. This will offer experimental materials and bases for further researches on Cu and Anore-forming laws and ore prognosis.