中文摘要:阳西脉岩蚀变型高岭土矿体受阳山逆掩断层的控制。高岭土主要矿物成分为1T高岭石、7A埃洛石及石英，并含少量叶腊石、地开石、绢云母、黄铁矿、方铅矿及闪锌矿等。根据矿床地质特征、矿物组合、成矿物理化学条件等讨论，高岭土矿床形成于中低温、中压、酸性、还原的介质条件。其主要成矿作用为与岩浆活动有关的热液作用。
Abstract:The Yangxi dike alteration type kaolin deposit is controlled by Yangxi overthrust. ln the area, wall-rock alterations are well developed and exhibit zonation. Main mineral composition of kaolin includes lT kaolinite, 7 A halloysite and quartz as well as small amounts of pyrophyllite, sericite, dickite, pyrite, galena and sphalerite. The protolith of kaolin is chiefly syenite porphyry. According to inclusion and sulfur stable isotope geothermometer, the ore-forming temperatures are 170~300℃, and the ore-forming depth is 3 280 m or so. The calculated physical-chemical parameters of the hydrothermal ore-forming stage are as follows: lgfS2 = -10.46; lgfO2 = - 31. 37; lgfCO2 = - 22. 77; lgfH2O= -7.54; lgaH2S= -21.58; lgaHSO4-= -31.92; lgaSO42-= -34.01. The ore-forming media are in a reduction environment. The ore-forming hydrothermal solution seems related to postmagmatic activity of intermediate-acid intrusives, being acid hydrothermal solution with rich CO2CL- and poor SO42-. The channelway for the migration of hydrothermal solution is mainly the faulted zone. It can be inferred from the above discussion that the Yangxi dike alteration type kaolin deposit must have been formed through the hydrothermal alteration of syenite porphyry in acid and reducing media under the action of mesothermal-epithermal solution related to the activity of intermediate-acid magma, with the superimposition and transformation of subsequent weathering-leaching.
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易发成，田煦，李虎杰，郑自立.1996.苏州阳西脉岩蚀变型高岭土矿床成因探讨[J].矿床地质,15(1):87~94.1996.A preliminary discussion on the genesis of the Yangxi dike alteration type Kaolin deposit Suzhou, Jiangsu Province[J].Mineral Deposits15(1):87~94
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