| 1. | What does the terrigenous sediment consist of ?
陆源沉积物是由什么组成的？
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| 2. | Grain - size variations of terrigenous sediment sequences in the south okinawa trough
冲绳海槽南部沉积层序的粒度特征
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| 3. | Research thinking of high - resolution sequence stratigraphy about a terrigenous basin
浅谈陆相盆地高分辨率层序地层研究思路
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| 4. | On some problems of mesozoic terrigenous volcanic series in fujian , zhejiang and jiangxi provinces
闽浙赣中生代陆相火山岩系几个问题的探讨
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| 5. | In order to remedy this shortage , it was put forward that the frame of terrigenous elastic rocks should be expressed as the collaring rectangle instead of rectangle
对于陆源碎屑岩来说，这样既不能表示出其粒度变化情况，又不能反映出它形成时的沉积动力学特征。
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| 6. | The main control factors of carbonate of preservation for information of seawater are : a ) the components of original minerals ; b ) the primary porosity of rock ; c ) the content of terrigenous elastics of carbonate rocks
有如下3个主要控制因素： a )原始矿物组成； b )岩石的原生孔隙度； c )碳酸盐岩中陆源碎屑矿物的含量。
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| 7. | A great number of lherzolite xenoliths occurs within the volcanic clastics characterized by terrigenous central type eruption at tianyang , jiudouyang and yingfenglin of qingtongyang , of southern leizhou peninsula
摘要雷州半岛南部田洋、九斗洋及青桐洋的英峰岭等陆相中心式喷发的火山碎屑岩中，分布有大量的二辉橄榄岩包体。
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| 8. | Results the result on this sedimentary environment was an offshore terrigenous fresh water lake from permian of shiqanfeng formation marinecontinental transitional facies in the southern of north china
结果研究区地层自南西向北东呈现依次增厚的趋势，整体为北东方向倾斜的宽缓斜坡环境；砂岩分布特征指示物源来自南部隆起区和沉积中心在研究区以北地区。
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| 9. | The mn / sr value considers the mn content for control factors of cathodoluminescence and the relative content of the marine versus terrigenous elements . so the mn / sr ratio is the relatively comprehensive discrimination criterion for controlling the alteration of marine carbonate
Mn sr比值在考虑了控制碳酸盐阴极发光性的mn含量的同时，兼顾了海相和陆相元素的相对含量，因而是一种较全面的成岩蚀变性判断标准。
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| 10. | On the basis of the types of sand stone , light and heavy mineral associations , planimetric map of sedimentary facies and directions of palaeoflow , it is considered that detrital material of terrigenous deposit of chang6 - 8 oil - beds in this area come from southwest provenance , northeast provenance , west provenance and south provenance , respectively , which are the denudation area of huating - longxian county in southwestern , yinshan ancient land in the northern , the denudation area of yantong mountain and tongxin to the west of yangjiajuzi - yinjiacheng county and qinling ancient land in the southern
根据砂岩类型、轻、重矿物组合、沉积相带平面展布及古水流方向等特征的分析，认为研究区延长组长6 ? 8油层组陆源碎屑物质来自西南、东北、西部和南部四大物源区，分别为西南华亭?陇县一带剥蚀区，北部阴山古陆，西部的杨家咀子、殷家城以西的烟筒山、同心地区剥蚀区和南部秦岭古陆。
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