运用数理统计和地质统计学方法，从矿区地层岩性、构造、岩浆岩、矿体的空间分布等方面研究了墨江金厂金矿床金元素的空间富集规律。
In this paper, the spatial enrichment regularities of gold are studied from the spatial distribution of ore bodies, lithology, construction and magmatic rocks with the methods of statistics and geos.
首次从岩石学的角度探讨了区域构造岩浆活动史。
The authors also discuss the regional tectonomagmatism activity from igneous petrologic angles.
实例研究证实，磁组构学方法对于岩浆动力学，特别是岩体构造应力的属性分析非常有效。
This attempt demonstrates that the method of magnetic fabric is effective in the field of magma dynamics, especially for reconstruction of the stress a granite body experienced.
造山带火山岩石学研究的主要目的在于重溯造山带的构造-岩浆演化历史。
The study of volcanic rocks in orogenic belts aims mainly at retracing the tectono_magmatic evolutionary history of orogenic belts.
岩石学和地球化学特征揭示包体寄主岩为碧玄岩，岩浆没有经历明显分异和同化混杂作用。
Their petrological and geochemical characters suggest that the host rock of the xenoliths is basanite, and the magma has not experienced obvious differentiation and assimilatory contamination.
对其矿床地质特征、同位素地质学、矿床成因等方面研究，认为成矿物质来源具双重性，既有来源于地层，又有来自壳幔源岩浆。
Studies on geology, isotopes and metallogenesis indicate that the ore forming material derived from strata and magma derived from crust mantle.
将熔体包裹体数据和常规的岩石学、地球化学和实验岩石学信息综合一体，可以提高我们模拟岩浆作用过程的能力。
Combining melt inclusion data with conventional petrological and geochemical information and experimental petrology can increase our ability to model magmatic processes.
综合岩石学、地球化学和同位素等方面的对比研究，笔者认为八大石闪长质包体属于同源包体，为寄主花岗岩同源母岩浆经结晶分异作用形成的早期产物。
Petrologic, geochemical and isotopic studies prove that the Badashi dioritic enclaves are autoliths and the earlier products generated by crystal fractionation of the host granite parental magma.
近年来，流体动力学被广泛引入地质学，特别是岩浆岩石学领域，逐渐形成新的学科生长点。
Fluid dynamics has extensively been introduced in geology, especially in igneous petrology, causing creation of a new disciplinary growing point.
近年来，流体动力学被广泛引入地质学，特别是岩浆岩石学领域，逐渐形成新的学科生长点。
Fluid dynamics has extensively been introduced in geology, especially in igneous petrology, causing creation of a new disciplinary growing point.
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