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海南岛雷公墨(玻璃陨石)起源问题的初步探讨
引用本文:袁宝印. 海南岛雷公墨(玻璃陨石)起源问题的初步探讨[J]. 地质科学, 1981, 0(4): 329-336
作者姓名:袁宝印
作者单位:中国科学院地质研究所
摘    要:玻璃陨石(tektite)或称熔融石是一种天然玻璃,它的成因是目前陨石学研究中激烈争论的问题。雷公墨是玻璃陨石的一种,发现于海南岛及雷州半岛等地。

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收稿时间:1980-05-09
修稿时间:1980-05-09;

PRELIMINARY DISCUSSION ON THE ORIGIN OF LEI-GONG-MO (TEKTITES)
Yuan Baoyin. PRELIMINARY DISCUSSION ON THE ORIGIN OF LEI-GONG-MO (TEKTITES)[J]. Chinese Journal of Geology, 1981, 0(4): 329-336
Authors:Yuan Baoyin
Affiliation:Institute of Geology, Academia Sinica, Beijing
Abstract:The specimens of Lei-gong-mo (tektites) which form the object of the present study were collected from Hainan Island and Leizhow Peninsula during the period from 1963 to 1975.The distribution,forms,sculpture,abration surface (bald spot),internal structure and chemical composition of Lei-gong-mo are discussed and the studies of these materials lead to the following conclusions :1.The specimens of Lei-gotig-mo so far known can be morphologically divided into eight types.2.The sculptures on the surface of Lei-gong-mo are formed probably due to the corrosion effect of volcanic gas on it,and the abration surface due to the aerodynamic corrosion.3.The folded structures in the layered Lei-gong-mo (Muong Nong-type tektite) seem hardly to be formed by an impact of meteorites,but they might be produced in the flow process of magma when the Lei-gong-mo was melting within the crater vent.4.The comparison of its chemical composition with that of basalt from Hainan Island does not show that Lei-gong-mo came from the local volcano.Based on the studies mentioned above,the author is inclined to agree with the hypothesis of the lunar volcanic origin of tektites.
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