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200年前詹姆士·赫屯正好化了两年时间寻找野外证据,用以支持他在1785年提出的观点——花岗岩是由注入到冷的主岩中的炽热岩浆通过结晶作用形成的.当他在苏格兰寻找主要的证据时,他正确地推想到不整合的重要性,并且收集了确信他的《地球理论》是正确的基本资料.最近,爱丁堡皇家学会和伦敦皇家学会在爱丁堡的赫屯城联合举办了一个题为花岗岩成因的国际会议庆祝这两百周年.
200 years ago, Jacinto Tun Tun just took two years to find field evidence in support of his point of view in 1785 that granites were formed by the crystallization of hot magma plumes into cold host rocks. When he was looking for the main evidence in Scotland, he rightly assumed the importance of disunity and gathered the basic information that convinced him that “earth theory” was correct.Recently, the Royal Society of Edinburgh and the Royal Society of London in Edinburgh Tuen Mun jointly organized an international conference entitled The Origin of Granites to celebrate the bicentenary.