中国东部新生代玄武岩中单斜辉石巨晶的主要特征及成因信息
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The Main Characteristics and Genetic Information of Clinopyroxene Megacrysts in Cenozoic Basalt of Eastern China
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    摘要:

    作者通过对我国东部新生代玄武岩中巨晶Cpx的109个样品的化学成分的统计、计算及投影,研究了Cpx巨晶的产状、物性及矿物化学的主要特征,并对其成因信息提出了自己的看法。Cpx巨晶的成分以A12O3、A1~(v1)较高而Ti、Mg'中等为特征。但在“反应边”中,A12O3、Na2O、A1、A1~(v1)则明显降低。我国巨晶以普通辉石为主,而透辉石、次透辉石及顽透辉石少见。国内不同地区的Cpx巨晶成分也略有不同:华南区巨晶的Wo较高而A1_2O_3较低;华北区Fs、A12O3较高;而东北区En较高而A1_2O_3中等。有关Cpx巨晶的成因信息,作者的观点是:(1)巨晶Cpx是寄主玄武岩浆在上地幔中结晶的产物,而不是地幔解体的捕虏晶。(2)我国巨晶Cpx的结晶温度是1021—1209℃,压力为1.4—3.2GPa,所以,Cpx巨晶的结晶深度为48—104Km。(3)我国东部新生代玄武岩均产于大陆板块内部,以碱性玄武岩成分为主,而拉斑玄武岩较少。

    Abstract:

    In this study, 109 chemical compositions of clinopyroxene (Cpx) megacrysts were collected from Cenozoic basalts in eastern China. The main characteristics of the. occurrence, physical properties and mineralogical chemistry of the Cpx megacrysts are studied 1 liy. means of large amounts of calculations and projec- tions. The authors present in this paper their own views on the genetic informa- tion of Cpx megacrysts. The compositions of megacrysts were characterized by higher contents of Al2O3 and Al(v1) and moderate Ti and Mg'. But in the "reaction rim" the contents of A1203 Na20, A1 and Al(v1) obviously decreased. The main species of Cpx megac- rysts is augite, while diopside, salite and endiapside are rare. And, the composi- tions of Cpx megacrysts are somewhat varied in .different regions of China.In southern China,the content of Wo' is relatively high with lower A1203; in the north, .Es and Al2O3 are higher; while in the northeast En is higher with mode- rate A1203. The opinions of the authors concerning the genetic information of Cpx me- gacrysts are; 1. The Cpx megacrysts are the products of crystallization of the host basal- tic magma in the upper mantle, but not xenocrystals derived from mantle disin- tegration. 2. The crystallization temperature and pressure of CpX megacrysts in China are 1021-1209℃and 1.4-3.2 Gpa respectively. Therefore the depths of Cpx me- gacrysts crystallization are approximately 48-104 km. The depth is shallower in southern China,deeper in northeastern China and deepest in northern China. The "reaction rim" was formed. at amore shallower mantle`=crust depth. 3. The Cenozoic basalts in eastern China all occur within the continental plate, dominated by alkalibasalts,with little tholeiite the basalts in areas along the basalts, since regions are close marginal sea.

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邱家骧,廖群安,1987,中国东部新生代玄武岩中单斜辉石巨晶的主要特征及成因信息[J].岩石矿物学杂志,6(1):56~64. Qiu Jiaxiang Liao Qunan,1987,The Main Characteristics and Genetic Information of Clinopyroxene Megacrysts in Cenozoic Basalt of Eastern China[J]. Acta Petrologica et Mineralogica,6(1):56~64.

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