inference of the three_dimensional geometry of the linglong granitic complex at depth from 2_d gravity forward modeling, constrained by geological data, shandong province, east china, is presented.
根据胶东地区西北部的重力资料 ,并在地质资料的约束下 ,采用人 -机联作的二维模拟方法 ,对玲珑花岗质杂巖体三维形态进行了细致的推断 。
the study of lead isotope has further p(?) ved that the weiya granitic complex is syntexjs series derived from mixing source of the mantle and crust.
铅同位素的研究进一步证明尾亚杂巖体系幔-壳混合源的同熔系列花岗巖。
the gutian-xiaotao granitic complex is composed of the xiaotao, gutian, huajia, jiaoyang and gutian units.
古田-小陶花岗质杂巖体是由小陶、古田、华家、蛟洋和姑田等单元组成。
linglong granitic complex is a polyphase composite rock body, emplaced finally in yenshan stage.
玲珑花岗质杂巖是一个多期次形成的复式巖体,最终定位于燕山期。