| 再论矿床的成矿系列问题 |
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| 引用本文： | 程裕淇,陈毓川,赵一鸣,宋天锐.再论矿床的成矿系列问题[J].地球学报,1983,5(2):1-64. |
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| 作者姓名： | 程裕淇 陈毓川 赵一鸣 宋天锐 |
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| 作者单位： | 中国地质科学院;中国地质科学院矿床地质研究所;中国地质科学院矿床地质研究所;中国地质科学院地质研究所 |
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| 摘 要： | <正> 在“初论矿床的成矿系列”一文中,作者等曾就矿床成矿系列这个概念形成的过程、提出的依据、包含的内容、在矿床学和成矿规律研究中的地位、它的可能的理论和实际意义等等,作了一定的论述,给它下了一个初步的定义;并以较多的篇幅,对在一定时期内,那些成矿物质(元素)富集成为矿床的作用直接同岩浆活动有关的十二个成矿系列的实例,分别进行了不同程度的叙述和分析,或就有关问题作了一些讨论。因限于资料搜集或研究程度的局限性,对于与沉积(成岩)作用有关的、以及(受)变质和变成矿床中建立的成矿系列有关问题,只分别提出了简略的意见,并分析了个别系列的实例。
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FURTHER DISCUSSION ON THE PROBLEMS OF MINEROGENETIC SERIES OF MINERAL DEPOSITS |
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| CHENG Yu-qi,CHEN Yu-chuan,ZHAO Yi-ming and SONG Tain-rui.FURTHER DISCUSSION ON THE PROBLEMS OF MINEROGENETIC SERIES OF MINERAL DEPOSITS[J].Acta Geoscientia Sinica,1983,5(2):1-64. |
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| Authors: | CHENG Yu-qi CHEN Yu-chuan ZHAO Yi-ming and SONG Tain-rui |
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| Institution: | Chinese Academy of Geological Sciences;Institute of Mineral Deposits, Chinese Academy of Geological Sciences;Institute of Mineral Deposits, Chinese Academy of Geological Sciences;Institute of Geology, Chinese Academy of Geological Sciences |
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| Abstract: | The classification of minerogenetic series is based on synthetic studiesof the geological conditions under which various types or type-groups of mineral deposits are formed. Above all, such series may be divided into threemajor groups as according to the geological setting of mineralization concernedcomparable to that of the formation of three major rock types. The main factors to be considered in the dividing of the first majorgroup, i. e., the magmatominerogenetic series association of the magmato-genic mineral deposits, into fifteen series (Table 1, English abstract;Table 3,Chinese text) are the acidity (basicity) and/or alkalinity and mode of occurrence of the magmatic rocks concerned, including whether the volcanic seriesare marine or/and continental, and also their geotectonic setting and othergeological conditions. The chief basis, on which the second, the sedimento-minerogenetic series association,or the minerogenetic series association geneticallyrelated to the process of sedimentation and also of diagenesis, is further classified into seven series (Table 2, English abstract; Table 4, Chinese text),is the litho-palaeogeographic features of the sedimentational epoch concerned,with due consideration also given to other factors such as geotectonic, climatic, geochemical, hydrodynamic, etc. for the subdividing of certain series anddiscussing some related geological problems. As for the third group, i. e.,mineral deposits of metamorphic terrains, its subdivision into five metamorpho-minerogenetic series (Table 3, English abstract; Table 5, Chinese text)is based upon the characters of relevant pre-metamorphic formations as wellas nature and degree of metamorphism. But transitional series between thesethree minerogenetic series associations have also been found. Certain minerogenetic series were formed only at certain geological periods and thus reflect in a way some characteristics of such evolutional epochsof the earth, such as the predominance of banded iron ore sub-series (sub-series "a" of the ME-1 minerogenetic series of Table 3 of this abstract) inArchean and early Proterozoic times, the frequent occurrence of the "polymatal" marine black shale, "coal-stone" (and siliceous rocks) association minerogenetic series of early Cambrian in certain regions of the world(S-7 M.S.,Table 2 of this abstract), etc. Minerogenetic series remoulded intensively by geological processes suchas metamorphism, magmatism and exogenesis with accompanying mineralizationof later minerogenotic epochs are often found in nature. But they should beclassified and named as according to the mineralization and minerogeneticepoch which have played the leading role in their coming into being. Having investigated the metallogeny of the rare earth-rare metal "coloured-metal"-minerogenetic series (Ma-1, Table 1 in this abstract or Table3 in the Chinese text) that related to the Yanshanian granites of medium-to shallow-depth emplacement of the Nanling region of South China throughan integrating analysis of the governing factors such as regional geology, geotectonics, magmatism, mineralization etc., four mineralization stages of theYanshanian metallogenetic epoch of the region in question have been recognized (Fig. 4, Chinese text) and hence four sub-minerogenotic series havebeen subdivided, viz., W-TR-Nb-Ta sub-series W-Sn-Pb-Zn-Nb-Ta-Be sub-series, Sn-Pb-Zn-Cu-Sb-As-Hg sub-series and U series. This may serve as anexample to elucidate the leading factors to be considered for the furtherclassification of certain minerogenetic series. |
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