皖西学院学报
皖西學院學報
환서학원학보
JOURNAL OF WANXI UNIVERSITY
2014年
5期
86-90
,共5页
张广胜%郝李霞%谭绿贵%赵怀琼
張廣勝%郝李霞%譚綠貴%趙懷瓊
장엄성%학리하%담록귀%조부경
皖西大裂谷%凤凰台盆地%构造断裂%凤凰台组地层%外力作用
皖西大裂穀%鳳凰檯盆地%構造斷裂%鳳凰檯組地層%外力作用
환서대렬곡%봉황태분지%구조단렬%봉황태조지층%외력작용
Wanxi Rift%Fenghuangtai Basin%tectonic fracture%stratum of Fenghuangtai Group%external force
通过对大别山(六安)国家地质公园皖西大裂谷园区的地质地貌考察,以及对皖西大裂谷形态特征的实地调研和分析,初步得出其地学成因机制:①大别山构造抬升形成的山前盆地---凤凰台盆地构造是形成皖西大裂谷的构造背景;②凤凰台组砾岩与砂岩互层是其物质基础;③区域构造断裂是其形成的内在动力前提;④重力崩塌作用、流水作用以及风力作用等是其进一步不断深入侵蚀的外力基础。对皖西大裂谷地学形成机理的探究,有助于大别山(六安)国家地质公园地学科普价值的实现和提高。
通過對大彆山(六安)國傢地質公園皖西大裂穀園區的地質地貌攷察,以及對皖西大裂穀形態特徵的實地調研和分析,初步得齣其地學成因機製:①大彆山構造抬升形成的山前盆地---鳳凰檯盆地構造是形成皖西大裂穀的構造揹景;②鳳凰檯組礫巖與砂巖互層是其物質基礎;③區域構造斷裂是其形成的內在動力前提;④重力崩塌作用、流水作用以及風力作用等是其進一步不斷深入侵蝕的外力基礎。對皖西大裂穀地學形成機理的探究,有助于大彆山(六安)國傢地質公園地學科普價值的實現和提高。
통과대대별산(륙안)국가지질공완환서대렬곡완구적지질지모고찰,이급대환서대렬곡형태특정적실지조연화분석,초보득출기지학성인궤제:①대별산구조태승형성적산전분지---봉황태분지구조시형성환서대렬곡적구조배경;②봉황태조력암여사암호층시기물질기출;③구역구조단렬시기형성적내재동력전제;④중력붕탑작용、류수작용이급풍력작용등시기진일보불단심입침식적외력기출。대환서대렬곡지학형성궤리적탐구,유조우대별산(륙안)국가지질공완지학과보개치적실현화제고。
Through investigation and analysis of the morphological characteristics of Wanxi Rift at Dabie Mountains (Lu'an) National Geological Park in West Anhui ,and also through investigation and analysis of morphological characteristics the Wanxi Rift ,obtained preliminary the geoscience formation mechanism :① Fenghuangtai Basin is the tectonic setting of Wanxi rift ,which formed by the tectonic lifting of Dabie Mountain and formed the foreland basin;② Cross layer of conglomerates and sandstones in Fenghuangtai Group stratum is the material base;③ Regional fault is the premise of the formation of intrinsic motivation ,④ the gravity collapse effect ,water and wind action are the effect of the continuously deep invasion force further erosion basis .On the formation of Wanxi Rift mechanism inquiry ,contribute to the Dabie Mountains (Lu'an) implementation and promotion of the National Geological Park to learn science value .