贵州云台山岩石特征及其峰丛—峰林地貌成景意义          下载免费PDF全文

龙建喜  谯文浪  王波  刘贞才 《贵州地质》2014,31(4):297-301

云台山峰丛—峰林的成景岩石主要为白云岩和（含）灰质白云岩,灰岩仅在峰丛—峰林基坐部分见及。成景岩石结构主要为颗粒结构和晶粒结构,且颗粒结构（颗粒和填隙物）、晶粒结构（晶粒白云石和少量泥质、少量陆源碎屑）在空间上各自顺层偏集呈层分布。此外,白云岩孔隙发育,孔隙类型有孔洞和裂隙两种,区内构造运动改造了原来的孔隙,加宽、加深其横纵向展布,增强孔隙的连通性,使原来较细级孔隙相互贯通成较大一级孔隙网,在水的溶蚀及机械崩塌等地质作用下成景。  相似文献   

Last Deglaciation Climatic Fluctuation Record by the Palaeo-Daocheng Ice Cap,Southeastern Qinghai-Tibetan Plateau     

ZHANG Zhigang  XU Xiaobin  WANG Jian  ZHAO Zhijun  BAI Shibiao  and CHANG ZhiYang 《《地质学报》英文版》2014,88(6):1863-1874

The last deglaciation, a key period for understanding present and future climate changes, has long been the hot topic for palaeoclimatological study. The Qinghai-Tibetan Plateau(QTP) is often a target study area for understanding hemispheric, or even global environment changes. The glacial landforms on the QTP provide a unique perspective for its climate change. In order to investigate the onset of the last deglaciation at the QTP and its regional correlation, the terrestrial cosmogenic nuclides(TCN) 10 Be and 26 Al surface exposure dating was chosen to date the roche moutonnée, the polished surface and the moraine debris located at the palaeo-Daocheng Ice Cap(pDIC), southeastern QTP. Our results show that the onset of the last deglaciation is at about 19 ka, followed by another warming event occurring around 15 ka in the p-DIC area. These timings agree well with other records, e.g. equivalent with a rapid sea level rise at 19 ka and the onset of B?lling warming event at about 15 ka. Thus, our new data can provide good reveal constraint on the climate evolution at the QTP.  相似文献   

塔里木盆地中央隆起中部中下奥陶统白云石类型及形成机理     

何洧  刘亿  姚城  徐梅桂  范筱聪 《海相油气地质》2013,(1):59-66

根据岩心及薄片观察,按照矿物晶体的大小、形状以及自形程度的差异,将塔里木盆地中央隆起中部中下奥陶统碳酸盐岩地层中的白云石分为6种类型,包括泥微晶白云石、粉—细晶自形—半自形漂浮状白云石、粉—细晶半自行—他形白云石、粉—细晶自形(环带)白云石、细—粗晶他形白云石、粗晶鞍形白云石。综合不同类型白云石的结构特征、碳氧锶同位素值、阴极发光等特征,认为中下奥陶统白云石主要由三种成岩作用形成:泥微晶白云石主要是在准同生期由回流白云石化形成;大部分粉—粗晶白云石是在埋藏期由埋藏白云石化形成,其中浅埋藏期是大规模白云石化的阶段;粗晶鞍形白云石主要由与高温热液活动相关的热液白云石化形成。  相似文献   

ZY-3 MUX传感器数据的缨帽变换系数推导     

施婷婷  徐涵秋  王帅 《遥感学报》2019,23(3):514-525

缨帽变换是一种实用性都很强的遥感影像增强方法,已被成功地应用于各种遥感领域。然而,对于缺少中红外波段的4波段高分卫星传感器,采用常规的Gram-Schmidt正交化方法难以推导出缨帽变换的湿度分量,即便少量推导出湿度分量的算法也存在着结果失真的问题。因此,开展针对4波段传感器缨帽变换系数的推导,提出了先确定湿度分量、再确定亮度和绿度分量的逆推算法,并将其应用在ZY-3 MUX传感器数据上。实验结果表明:(1)逆推方法可以有效地推导出ZY-3 MUX缨帽变换的湿度分量,较好地解决了前人研究中出现的湿度分量失真问题;(2)新方法求出的3个分量的散点在其三维特征空间中呈现典型的"缨帽"特征,较于传统的GramSchmidt正交化方法,新方法的散点在水体、植被和建筑用地/裸土之间的空间分布位置可以更好地相互分离,不会造成不同地类之间的混淆;(3)采用新方法所得到的缨帽变换系数的精度好于传统的Gram-Schmidt正交化方法,体现在新方法具有较高的R值和较低的RMSE误差。本研究可为ZY-3 MUX数据提供一套有效的缨帽变换系数,同时也为缺乏中红外波段的高空间分辨率遥感影像提供一种新的缨帽变换系数推导方法,解决了常规GramSchmidt正交化方法无法准确表示湿度分量的问题。  相似文献   

First period analyses of five neglected Algol-type eclipsing binaries: TT And, V342 Aql, RW Cap, BZ Cas and TW Lac     

A. Erdem  F. Soydugan  S.S. Doru  B. zkarde  D. Doru  M. Tüysüz  O. Demircan 《New Astronomy》2007,12(8):613-621

We present the first study of the orbital period variations of five neglected Algol-type eclipsing binaries TT And, V342 Aql, RW Cap, BZ Cas and TW Lac, using their O–C diagrams gathered from all available times of eclipse minima. These O–C diagrams indicate that short term periodic variations superimposed on secular period increases as expected in mass transferring Algols. However, due to short time coverage of the data, the secular period increase is not clear in the case of BZ Cas and V342 Aql. The secular period increase is interpreted in terms of the combined effect of mass transfer between the components of the system and the mass loss by a stellar wind from the system. The mass transfer rates from the less massive secondary components to the more massive primaries for non-conservative cases would be about 10⁻⁷M/yr and 10⁻⁸M/yr for RW Cap and V342 Aql, respectively, and 10⁻⁹M/yr for TT And and TW Lac. Therefore, the Algol systems RW Cap and V342 Aql have the largest mass transfer rate, which could be in Case AB type, while those of the Algol systems TT And and TW Lac display the slow mass transfer rate and they could be in Case B type. The sinusoidal forms of the orbital period variations of all five Algol systems can be due to either by the light-time effects due to unseen components in these systems, or by the cyclic magnetic activity effects of the cool secondary components. The possible third bodies in all five Algol binaries would have masses larger than one solar mass. If these hypothetical large massive third bodies were normal stars, they should be detectable. Therefore, new photometric and spectroscopic observations of these systems and careful analyses of those data are required. Otherwise, the cyclic magnetic activity effects of the secondary components could be the basis of a working hypothesis in explaining the cyclic period variations of these systems.  相似文献   

Multiple-scale facies and reservoir quality variations within a dolomite body – Outcrop analog study from the Middle Triassic,SW German Basin     

Bastian Simon Koehrer  Christian Heymann  Frank Prousa  Thomas Aigner 《Marine and Petroleum Geology》2010

This study focuses on a porous dolomite body in the proximal part of an epeiric carbonate ramp (Triassic Muschelkalk, South German Basin), analogous to hydrocarbon-bearing dolomite reservoirs in the Middle East (e.g. Khuff and Arab Formations).  相似文献   

Ice-marginal sedimentation associated with the Late Devensian Welsh Ice Cap and the Irish Sea Ice Stream: Tonfanau, West Wales     

Henry Patton  Michael J. Hambrey 《Proceedings of the Geologists' Association. Geologists' Association》2009,120(4):256-274

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Recently exposed vegetation reveals Holocene changes in the extent of the Quelccaya Ice Cap, Peru     

Aron M. Buffen  Lonnie G. Thompson  Ellen Mosley-Thompson 《Quaternary Research》2009,72(2):157-308

Radiocarbon dating of well-preserved, in-place vegetation exposed by the retreating Quelccaya Ice Cap of southeastern Peru constrains the last time the ice cap's extent was smaller than at present. Seventeen plant samples from two sites along the central western margin collectively date to 4700 and 5100 cal yr BP and strongly indicate that current ice cap retreat is unprecedented over the past ∼ 5 millennia. Seventeen vegetation samples interbedded in a nearby clastic sedimentary sequence suggest ice-free conditions at this site from ∼ 5200 to at least ∼ 7000 cal yr BP, and place minimum constraint on early- to mid-Holocene ice cap extent.  相似文献   

Thermochemical sulphate reduction in the Upper Devonian Cairn Formation of the Fairholme carbonate complex (South-West Alberta, Canadian Rockies): evidence from fluid inclusions and isotopic data     

VEERLE VANDEGINSTE  RUDY SWENNEN  SARAH A. GLEESON†  ROB M. ELLAM‡  KIRK OSADETZ§  FRANÇOIS ROURE¶ 《Sedimentology》2009,56(2):439-460

The Fairholme carbonate complex is part of the extensively dolomitized Upper Devonian carbonate reefs in west-central Alberta. The studied formations contain moulds (up to 10 cm in diameter), which are filled partially with (saddle) dolomite, quartz and calcite cements. These cements precipitated from a mixture of brines that acquired high salinity by dissolution of halite and brines derived from evaporated sea water. The fluids were warm (homogenization temperature of primary fluid inclusions of 76 to 200 °C) and saline (20 to 25 wt% NaCl equivalent) and testify to thermochemical sulphate reduction processes. The latter is deduced from S in solid inclusions, CO₂ and H₂S in volatile-rich aqueous inclusions and depleted δ¹³C values down to −26‰ Vienna Pee Dee Belemnite. High ⁸⁷Sr/⁸⁶Sr values (0·7094 to 0·7110) of the cements also indicate interaction of the fluids with siliciclastic sequences. The thermochemical sulphate reduction-related cements probably formed during early Laramide burial. Another (younger) calcite phase, characterized by depleted δ¹⁸O values (−23·9‰ to −13·9‰ Vienna Pee Dee Belemnite), low Na (27 to 37 p.p.m.) and Sr (39 to 150 p.p.m.) concentrations and non-saline (∼0 wt% NaCl equivalent) fluid inclusions, is attributed to post-Laramide meteoric water.  相似文献   

川东北飞仙关组白云岩的主要类型、地球化学特征和白云化机制   总被引：17，自引：9，他引：8  

黄思静  佟宏鹏  刘丽红  胡作维  张雪花  郇金来  黄可可 《岩石学报》2009,25(10):2363-2372

四川盆地东北部蕴藏有丰富的烃类资源,三叠系飞仙关组的白云岩是最主要的储层和产层,这使得飞仙关组白云岩成为人们近年来高度关注的对象.按照结构,我们可以将飞仙关组白云岩分为三种端元类型:微晶白云岩、具原始结构的粒屑白云岩和结晶白云岩,在一个向上变浅的剖面旋回中,这三种白云岩分别位于旋回的顶部、上部和中下部.微晶白云岩和具原始结构的粒屑白云岩具有较高的锰含量和较低的包裹体均一化温度,白云化流体的δ~(18O) 值(从白云石的包裹体均一化温度和δ~(18O) 值反演,以下同)介于大气水和海水之间,反映这类白云岩形成于有大气水参与的相对开放的沉积-成岩环境中,蒸发泵作用(对于微晶白云岩)和混合水作用(对于具原始结构的粒屑白云岩)可能是其主要的形成机制;结晶白云岩(表现为好储层)具有很低的锰含量和较高的包裹体均一化温度,白云化流体的δ~(18O) 值显著高于早三叠世海水,表明这类白云岩形成于相对封闭的埋藏成岩环境,白云化流体具较高的温度和盐度,但到目前为止,还没有一个已有模式可以较好地解释这类白云岩的成因.  相似文献