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希腊地质学家、岩石学家S.S.奥古士梯蒂斯教授应我冶金部邀请来我国参加中国地质学会60周年年会.会后在北京(部地质局)和桂林(部地质研究所)讲学,并考察了柿竹园钨矿、黄沙坪铅锌矿和大厂锡矿.继而赴南京大学讲学并参加南大主办的国际花岗岩研究会. 奥古士梯蒂斯是欧洲岩石学变成学派代表学者之一,层控矿床学者与该学派有密切联系.他在我国讲述了五个专题.①论花岗岩化;②铬铁矿的活化转移;③铝土矿的淋滤;④埃塞俄比亚火山岩;⑤普通辉石的振荡分带. 他认为花岗岩中变晶生长、变晶序列、次变边反应(蠕状化石)、后成合晶交生、文象结构、条纹长石化是认识
The Greek geologist and petrographer, Professor SS Augustus Teese, invited me to attend the 60th Anniversary of China Geological Society at the invitation of Ministry of Metallurgical Affairs. After the symposium, he gave lectures in Beijing (Department of Geology) and Guilin (Department of Geology) , And investigated the Shizhuyuan tungsten ore, yellow Shaping lead-zinc mine and Dachang tin mine, then went to Nanjing University to lecture and attend the International Granite Association sponsored by Nanda. Austrian disabilities Shi Teisi is the European petrology into a school representative One of the scholars, stratabound mineral deposit scholars and the school are closely linked.He told about five topics in our country.① On graniticization; ② Activation and transfer of chromite; ③ Bauxite leaching; ④ Ethiopian volcanic rocks; ⑤ Ordinary pyroxene oscillation zone.He believes that the granite in the growth of metamorphic, metamorphic sequence, the second variable edge reaction (fossil fossils), after the formation of crystal cross, the image of the structure, striped feldspar is understanding