2) Huaiyang Depression
淮阳坳陷
1.
Accumulation condition and exploration direction of Permo-Carbon-iferous system,Huaiyang Depression;
淮阳坳陷石炭—二叠系成藏条件与勘探方向选择
3) Beihuaiyang
北淮阳
1.
Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.
北淮阳盆岭构造带是大别造山带的重要组成部分。
2.
By means of different subjects and te chniques,the paper makes an overall study on the crustal stability of Beihuaiyang region and its adjace nt areas from the aspects of current t ectonic stress fields,principal fa ult structures,analysis of regional fa ults and neotectonic activity,seis mic activity and numerical modeling,etc.
运用多学科、多技术相结合的研究方法,从现今构造应力场特征、现代地壳形变特征、主干断裂构造以及区域断裂活动性分析、新构造运动、地震活动、数值模拟等方面入手,对北淮阳及其邻接区地壳稳定性进行了全面而系统的研究,指出本区地震活动受走滑活动断裂控制,中、强地震集中于区内东南部和西北部NW向与NE向断裂交汇处;第四纪无大规模差异升降运动;数值模拟等综合分析表明,信阳地区的区域构造稳定性高,现代地壳形变量小,应力平缓,地震活动少且弱。
4) North Huaiyang
北淮阳
1.
The timing and tectonic implications for the North Huaiyang synclinoria;
安徽北淮阳复向斜形成时间及其构造意义
2.
Geochemical characteristics of Yanshanian magmatic rocks in north Huaiyang and their tectonic environment;
北淮阳燕山期岩浆岩地球化学特征及其构造环境
3.
This paper briefly introduced the current research situation of stratigraphy,tectonics,magmatic rocks and other geological aspects as well as some major geological issues in the North Huaiyang area.
简要介绍了北淮阳地区地层、构造、岩浆岩等基础地质方面的研究现状及存在的一些主要地质问题,并对该区的基础地质研究方向进行了探讨,认为加强区域基础地质研究,探索区域成矿地质条件和成矿规律是区域矿产勘查工作的基
5) Northern Huaiyang
北淮阳
1.
Petrological and geochemical characteristics of Mesozoic adakite from Northern Huaiyang and discussion on its genesis.;
北淮阳中生代adakite岩石地球化学特征及成因讨论
2.
The discovery of UHP minerals and HP UHP metamorphic belt in Dabie Mountains has stimulated the strategraphy researth in Northern Huaiyang belt.
总结了近年来北淮阳地区地层研究的新进展 ,即确定了西段桐柏地区寒武系地层 ,厘定了中段南湾组与定远组形成时代 ,再次划分了东段佛子岭群与梅山群地层层序。
3.
Mesozoic thrusting in northern Huaiyang region, in northern edge of Dabieshan, caused mid to shallow metamorphic structural strata of mainly Early Paleozoic age, widely developed in the area and extending over several hundreds of kilometers, to overthrust NE ward on rocks of Carboniferous and Jurassic ages.
大别山北缘北淮阳地区中生代逆冲推覆构造作用使本区广泛发育的以下古生界为主体的中、浅变质构造地层，在数百公里的范围内向ＮＥ逆冲（掩）于石炭系和中侏罗统之上，形成一系列构造窗、飞来峰和逆冲（掩）断层带，其最小逆冲推覆距离平均为２４４ｋｍ，形成时代介于Ｊ２—Ｊ３之间，其形成与大别造山带的碰撞挤压有关，是大别地块中生代向北仰冲作用的结果。
6) modern Huaiyang
近代淮阳
1.
The grass-roots folk organizations in modern Huaiyang country and their transformation;
近代淮阳乡村基层民间组织及嬗变
补充资料：淮阳病
1.见"淮阳多病"。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条