|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | 四川盆地深层微生物碳酸盐岩储层特征及其油气勘探前景显示文摘微生物碳酸盐岩是油气勘探储层的新类型。四川盆地微生物碳酸盐岩储层主要发育在上震旦统灯影组和中三叠统雷口坡组。灯影组微生物碳酸盐岩储层主要发育在灯二段和灯四段。灯影组微生物碳酸盐岩遍布全盆,岩石结构具有全盆地相似性,灯二段以凝块石和葡萄石为主,灯四段以纹层石和叠层石为主。灯二段储集空间主要为喀斯特孔洞、葡萄-花边状孔洞、微生物体腔孔、微生物格架间孔和凝块间溶孔,灯四段则以窗格孔和喀斯特孔洞为主。灯影组微生物碳酸盐岩优质储层形成的主控因素是微生物席、白云石化和风化壳喀斯特作用。雷口坡组微生物碳酸盐岩主要分布在川西地区的雷四段,主要为叠层石和凝块石,储集空间主要为微生物窗格孔和格架孔。雷口坡组微生物碳酸盐岩优质储层形成的主控因素是微生物礁滩(微生物席)、白云石化和埋藏溶蚀作用。目前,在灯影组和雷四段微生物碳酸盐岩储层均已发现大型气田,并具有非常广阔的勘探前景。四川盆地西部中北段是深层-超深层海相领域油气勘探的最有利地区之一。 | 刘树根 宋金民 罗平 QING Hairuo 林彤 孙玮 李智武 王浩 彭瀚霖 余永强 龙翼 万元博 | 2016 | 成都理工大学学报(自然科学版)2016，43，2： | 67 |
| 2 | 青藏高原北缘酒泉盆地青西凹陷白垩系湖相热水沉积原生白云岩显示文摘通过岩相学、组构学和地球化学的综合研究,详细描述和论证了一种独特而罕见的中生代断陷湖盆条件下,碱性热卤水结晶沉淀的纹层状泥晶原生含铁白云岩.主要造岩矿物为泥晶结构的含铁白云石,此类白云石多呈0.1~1 mm厚的纹层,并与钠长石、方沸石、重晶石和地开石等多种热液矿物呈两元或多元互纹层产出.岩石地球化学结果显示:富含Sb,Ba,Sr,Mn和V等热水沉积标型元素,LREE相对富集,具典型的负Eu异常稀土配分模式,氧同位素δ18OPDB介于-5.89‰^-14.15‰,平均-9.69‰,87Sr/86Sr比值介于0.711648~0.719546,平均0.714718,反映沉积环境为受基底断裂控制的稳定、封闭和缺氧的深湖底低洼热卤水池,热流体为下渗湖水与幔源岩浆水混合形成的富含Ca2+,Mg2+和Fe2+等多种离子的碱性热卤水,受岩浆热能驱动流、重力驱动流及压实驱动流共同作用,突破上覆沉积物和湖泊水体的静水负荷压力发生沸腾爆炸,将喷流口上覆先期的纹层状泥晶含铁白云岩震碎,形成'水爆角砾岩';在距喷流口较远的低洼、安静的热卤水池中,热液则快速结晶化学沉淀出纹层状泥晶原生含铁白云岩.该套特殊岩石的研究一定程度上将有助于推动湖相碳酸盐岩和白云岩成因研究,特别是为我国中、新生代同类盆地湖相白云岩研究提供新的范例和研究思路. | 文华国 郑荣才 HaiRuo QING 范铭涛 李雅楠 宫博识 | 2014 | 中国科学:地球科学2014，44，4： | 56 |
| 3 | 四川盆地东北部三叠系飞仙关组碳酸盐岩成岩作用和白云岩成因的研究现状和存在问题显示文摘四川盆地东北部三叠系飞仙关组是我国重要的天然气储集层,优质储层形成机制直接与碳酸盐岩成岩作用、尤其是白云岩化作用相关,但飞仙关组碳酸盐岩在锰含量、锶含量、阴极发光性等特征上反映其成岩过程与经典成岩理论相悖;碳酸盐岩的锶同位素组成和锰、锶含量的关系也表明与大气水有关的成岩过程和作为重要储集岩的结晶白云岩的形成机制无关,传统的白云岩化机制难以解释结晶白云岩的成因。具有海源色彩的高锶、低锰成岩流体在很大程度上控制了飞仙关组碳酸盐的成岩作用,其来源与成因值得进一步关注,控制其运移、封存和发生水—岩反应的时空机制有待回答。整个海相三叠纪时间段盆地尺度碳酸盐岩和蒸发岩的沉积地球化学研究、尤其是不同结构组分碳酸盐的锶同位素组成、锶和锰含量研究(包括碳酸盐岩中不同结构组分的阴极发光性研究),可为四川盆地东北部飞仙关组碳酸盐岩成岩作用(尤其是白云岩化作用和作为重要储集岩的结晶白云岩的成因研究),天青石矿床成因研究和四川盆地三叠系深层富钾、锶、硼、溴卤水的成因研究提供重要的线索。 | 黄思静 Hairuo QING 胡作维 王春梅 郜晓勇 邹明亮 王庆东 | 2007 | 地球科学进展2007，22，5： | 38 |
| 4 | 晚二叠世-早三叠世海水的锶同位素组成与演化--基于重庆中梁山海相碳酸盐的研究结果显示文摘测试了重庆中梁山剖面晚二叠世-早三叠世60个海相碳酸盐样品的锶同位素比值,建立了相应的演化曲线,同时分析了这些样品的SiO2,CaO,MgO,Mn和Sr含量,以评估样品锶同位素组成对海水的代表性以及样品溶解过程的合理性.除7个样品的Mn/Sr比值大于2,其锶同位素组成对海水的代表性相对较差以外,绝大多数样品的锶同位素组成对海水都具有较好的代表性.在已报道的晚二叠世-早三叠世海水的锶同位素演化曲线中,中梁山剖面是数据密度最大,曲线最为完整的.曲线总体演化趋势具有很好的全球一致性,^87Sr/^86Sr比值整体上呈现随时间变化单调上升的特征,最小值(0.707011)位于晚二叠世,最大值(0.708281)出现在早、中三叠世界线附近.全球古陆植被缺乏和风化作用加剧是早三叠^87Sr/^86Sr比值随时间单调上升的主要原因.重庆中梁山剖面二叠纪三叠纪界线是一个全球认可的界线,界线处6个样品的^87Sr/^86Sr比值仅在小数后第5位变化,其平均值为0.70714,与Korte等在2006年公布的0.70715(样品来自有铰腕足壳)的二叠系/三叠系界线处^87Sr/^86Sr比值一致(变化在实验误差范围内),因而提供的二叠系三叠系之交海水的锶同位素组成具有全球意义.可基本确认,二叠纪/三叠纪之交全球海水的^87Sr/^86Sr比值在0.70714-0.70715之间. | 黄思静 Hairuo Qing 黄培培 胡作维 王庆东 邹明亮 刘昊年 | 2008 | 中国科学(D辑)2008，38，3： | 35 |
| 5 | 四川盆地东北部三叠系飞仙关组硫酸盐还原作用对碳酸盐成岩作用的影响显示文摘四川盆地东北部三叠系飞仙关组存在广泛的硫酸盐还原作用,同时地层中也存在锶含量异常高的成岩流体。研究表明:热化学硫酸盐还原作用(TSR)和(或)细菌硫酸盐还原作用(BSR)造成的SO42-离子的消耗对成岩孔隙流体中SrSO4溶解度的改变是三叠系中高Sr成岩流体的形成机制之一,该机制使得孔隙流体从白云石化作用和碳酸盐矿物的新生变形作用中获得的Sr在流体中以高浓度的Sr2+形式存在,并使之在流体中极度富集,这也是四川盆地东北部三叠系中大型和超大型天青石矿床的形成机制之一。H2S和CO2是硫酸盐还原作用的重要产物,不同温度条件下溶于水中的H2S和CO2,与不溶于水的气体分子之间的平衡反应H2S(aq)H2S(g)和CO2(aq)CO2(g)的平衡常数和吉布斯自由能增量计算表明,当温度从25℃升高至220℃时,两个反应的平衡常数分别大致从10增至240和从20增至500,两个反应的平衡常数都始终大于1,说明H2S和CO2更趋向于以气体形式存在,同时温度越高,系统中以气体形式存在的H2S和CO2会越多,溶解于水中的H2S和CO2会越少,因而在深埋藏的高温条件下,H2S和CO2对碳酸盐矿物的溶解能力可能相对很小。相对低温的成岩环境、高温流体的向上和侧向运移、构造抬升、富氧流体与含有H2S流体的混合以及金属硫化物的沉淀是提高含H2S和(或)CO2流体对碳酸盐矿物溶解能力的五个途径。因此,与较早成岩阶段相对浅埋藏环境的碳酸盐溶解作用有关的H2S和CO2流体可能与细菌硫酸盐还原作用(BSR)关系更为密切;断层或其它流体运移通道是高温含有H2S和CO2流体向上运移的基础条件,具有原生孔隙度和渗透率的礁、滩相高能沉积物也是流体发生侧向运移的先决条件;大幅度的构造抬升造成的地层温度降低是提高含H2S和(或)CO2地层流体对碳酸盐矿物溶解能力的重要因素,地壳抬升至近地表造成的古喀斯特作用也可以为H2S的氧化提供良好的地质环境。在有关的勘探中应注意:在断层等流体运移通道造成高温含H2S和CO2流体向上运移的条件下,与之有关的构造低点应该是主要的勘探目标;在燕山运动导致的地层抬升并导致深部热流体降温的条件下,与之有关的构造高点应该是主要的勘探目标,应分别对待。 | 黄思静 Hairuo Qing 胡作维 邹明亮 冯文立 王春梅 郜晓勇 王庆东 | 2007 | 沉积学报2007，25，6： | 34 |
| 6 | 川西致密砂岩的石英次生加大及其对储层的影响显示文摘石英次生加大以及伴生的自生粘土矿物是影响储层性质的重要因素。石英次生加大是受温度控制的成岩矿物,随着温度的升高,石英次生加大的含量也随之增加,导致孔隙度的降低。钾长石和高岭石在温度>90℃反应形成的伊利石,造成了储层渗透率的降低。本文通过对石英次生加大产出特征和流体包裹体温度的研究,进而讨论川西香溪群致密砂岩储层的成因。 | 张哨楠 Hairuo Qing K.Bjorlykke | 1998 | 地质论评1998，44，6： | 26 |
| 7 | Evolution of strontium isotopic composition of sea-water from Late Permian to Early Triassic based on study of marine carbonates,Zhongliang Mountain,Chongqing,China显示文摘Collected from a Late Permian to Early Triassic sedimentary section in the Zhongliang Mountain of Chongqing, Southwest China, sixty marine carbonate samples were measured for the 87Sr/86Sr ratios, and corresponding evolution curve was constructed. The concentrations of SiO2, CaO, MgO, Mn and Sr are used to evaluate reservation of strontium isotopic composition for original seawater and the credi-bility of the dissolution method for sample preparation. The results show that most of the samples (except seven samples with the Mn/Sr ratios higher than 2) contain the original geochemistry signa-tures of ancient seawater. Compared to the published 87Sr/86Sr ratios from the Late Permian to Early Triassic, our database reported here is the largest and the curve constructed is the most complete. The strontium isotopic curve from Late Permian to Early Triassic is consistent globally and exhibits a gen-eral trend of steady increase during this period. The minimum of 87Sr/86Sr ratios (0.707011) occurs in the Late Permian (30 m in thickness below the Permian-Triassic boundary), and the maximum (0.708281), near the Early-Middle Triassic boundary. The lack of land plants and the rapid continental weathering result in the increase of 87Sr/86Sr ratios during the interval. The Permian-Triassic boundary in Zhongli-ang Mountain Section has been accepted internationally. The 87Sr/86Sr ratios of six samples near the boundary vary from 0.70714 to 0.70715 with an average of 0.70714, which is consistent with the value of 0.70715 (samples are from articulate brachiopod shells) from Korte et al. published in 2006 (within the error range in experiment). Accordingly, the strontium isotope composition in the Permian-Triassic boundary in this paper is of global significance. It can be confirmed that the 87Sr/86Sr ratios of the sea-water in the Permian-Triassic transition are in the range of 0.70714―0.70715. | HUANG SiJing Qing HaiRuo HUANG PeiPei HU ZuoWei WANG QingDong ZOU MingLiang LIU HaoNian | 2008 | Science China Earth Sciences2008，51，4： | 24 |
| 8 | 酒泉盆地青西凹陷下沟组湖相热水沉积岩流体包裹体特征显示文摘以地质背景和岩石组构分析为基础,系统研究了酒泉盆地青西凹陷下沟组湖相热水沉积岩中的流体包裹体特征。结果表明,热水沉积岩中的原生流体包裹体以气液二相包裹体为主、单一液相和单一气相包裹体较少、偶见含子矿物三相包裹体。成矿流体属NaCl-H2O型热液体系,温度为90~200℃,盐度为8%~22%NaCl,密度为0.99~1.2g/cm3,成矿压力为15~180MPa。结合锶同位素等地球化学资料分析,认为成矿流体属于深循环的下渗湖水与岩浆水共同构成的中低温、中高盐度和中偏高密度混合热卤水。提出以不同产状的重晶石、铁白云石和萤石为代表的热水沉积岩的成矿热流体系统,自主喷流通道、分支喷流通道经喷流口至附近及远端的盆地热卤水沉积区存在温度、盐度、密度和压力等物理化学参数逐渐降低的分带性变化规律。在热流体特征分析基础上,对研究区早白垩世湖底热流体成矿机制和成因模式进行了探讨。 | 文华国 郑荣才 Hairuo QING 范铭涛 汪满福 | 2010 | 地质学报2010，84，1： | 15 |
| 9 | 酒泉盆地青西凹陷下沟组湖相热水沉积岩锶同位素地球化学特征显示文摘以地质背景、物质组分和岩石组构分析为基础,对酒泉盆地青西凹陷下沟组湖相热水沉积钠长石—铁白云石岩进行了Sr同位素地球化学研究。结果表明,热水沉积岩87Sr/86Sr比值变化范围为0.71225~0.71781,平均值0.71561,远高于同期海水和下沟组玄武岩,略高于代表早白垩世湖水锶同位素组成的藻灰岩,但低于基底壳源硅铝质岩,反映热流体不可能为单纯的湖水或幔源岩浆水;其中直接化学结晶沉淀的纹层状泥微晶热水沉积岩锶同位素比值变化范围较小,可代表均一化的热卤水池流体锶同位素组成特征;指示不同喷流口位置的'水爆角砾岩'锶同位素组成变化较大,但同一位置的热水角砾与胶结物锶同位素组成基本一致,说明两者应属于具相同成因意义的同期热水喷流沉积产物;综合青西凹陷下沟组湖相热水沉积岩锶同位素地球化学特征,初步推测早白垩世湖底热流体可能为富集硅铝质基底岩石高放射成因Sr的深循环下渗湖水与少量上升幔源岩浆水构成的混合热流体,可为青西凹陷早白垩世湖底热流体性质的确定以及热流体循环动力学模型和热水沉积模式的建立奠定基础。 | 文华国 郑荣才 Hairuo Qing 吴国瑄 夏佩芬 陈浩如 廖一 | 2009 | 沉积学报2009，27，4： | 12 |
| 10 | Primary dolostone related to the Cretaceous lacustrine hydrothermal sedimentation in Qingxi sag, Jiuquan Basin on the northern Tibetan Plateau显示文摘Based on comprehensive studies in petrography,petrofabric analysis and geochemistry,this paper describes a unique and rare laminated micritic ferruginous primary dolostone crystallized and precipitated from the alkaline hot brine under the conditions of the Mesozoic faulted lake basin.The main rock-forming mineral of this dolostone is ferruginous dolomite with a micritic structure.This dolomite mostly exhibits laminae of 0.1–1 mm thick and is often discovered with other minerals,such as albite,analcite,barite and dickite,which have at least two types of interbedded laminae.Petrogeochemistry reveals that this dolostone contains a large number of typomorphic elements of hydrothermal sedimentation,including Sb,Ba,Sr,Mn,and V.In addition,the LREE is in relatively high concentrations and possesses the typical REE distribution pattern with negative Eu anomaly.Oxygen isotope values(δ18OPDB)range from 5.89‰to 14.15‰with an average of 9.69‰.The ratio of87Sr/86Sr is between0.711648 and 0.719546,with an average of 0.714718.These data indicate that the depositional environment is a stable,blocked,anoxic low-lying hot brine pool in the bottom of deep lake controlled by basement faults.The hydrothermal fluid is the alkaline hot brine formed by the combination of the infiltration lake water and mantle-derived magmatic water,consisting of many ions,including Ca2+,Mg2+and Fe2+.Under the driving flow power of magmatic heat,gravity and compaction,the hydrothermal fluid overcame the overburden pressure and hydrostatic pressure of the lake water body,and boiled to explosion,and then the explosion shattered the original laminated micritic ferruginous primary dolostone near the vent and then formed a new type of dolostone called shattered'hydroexplosion breccias'.In the low-lying,unperturbed hot brine pool,far from the vent,the laminated micritic ferruginous primary dolostone was quickly crystallized and chemicals precipitated from the hydrotherm.This study of special rocks contributes to research into the causes of the formation of lacustrine carbonate rocks and dolostone.In particular,it provides new examples and research insights for future studies of the lacustrine dolomite from the similar Mesozoic and Cenozoic basins in China. | WEN HuaGuo ZHENG RongCai QING HaiRuo FAN MingTao LI YanAn GONG BoShi | 2013 | Science China Earth Sciences2013，56，12： | 12 |
| 11 | In situ stable isotopic constraints on dolomitizing fluids for the hydrothermally-originated saddle dolomites at Keping, Tarim Basin显示文摘Detailed characterization of diagenetic fluid behaviour and evolution is commonly hindered by shortage of appropriate and economic methods to carry out in situ analysis in the tiny diagenetic mineral crystals. Using micromill sampling method, this study presents in situ stable isotopic data for the growth zones of saddle dolomite crystals in the hydrothermally-altered dolostones of Upper Cambrian (Furongian) at Keping, Tarim Basin, NW China. These data show minor and large variations in δ13C ( 0.7‰ to 1.5‰ VPDB) and δ18O ( 8.3‰ to 13.8‰ VPDB), respectively, from the cores to outer rims of the dolomite crystals and suggest that saddle dolomites precipitated from dolomitizing fluids with similar carbon sources but oscillatory temperatures during different formation stages. This scenario is confirmed by microthermometry of fluid inclusions within the growth zones of dolomite crystals. This study indicates that in situ isotope analysis could provide more detailed information related to the source and pathway of dolomitizing fluids, facilitating better characterization of dolomitizing fluids and processes. | DONG ShaoFeng CHEN DaiZhao QING HaiRuo JIANG MaoSheng ZHOU XiQiang | 2013 | Chinese Science Bulletin2013，58，23： | 9 |
| 12 | WELL TESTING ANALYSIS FOR HORIZONTAL WELL WITH CONSIDERATION OF THRESHOLD PRESSURE GRADIENT IN TIGHT GAS RESERVOIRS显示文摘A fundamental solution for homogeneous reservoir in infinite space is derived by using the point source function with the consideration of the threshold pressure gradient. The fundamental solution of the continuous point source function is then derived based on the Green function. Various boundary conditions of the reservoirs are considered for this case and the corresponding solutions are obtained through the mirror image reflection and the principle of superimposition. The line source solution is obtained by integration. Subsequently, the horizontal-well bottom hole pressure response function for a non-linear gas flow in the homogeneous gas reservoir is obtained, and the response curve of the dimensionless bottom hole pressure and the derivative for a horizontal well in the homogeneous gas reservoir are obtained. In the end, the sensitivities of the relevant parameters are analyzed. The well test model presented in this paper can be used as the basis of the horizontal well test analysis for tight gas reservoirs. | GUO Jing-jing ZHANG Su ZHANG Lie-hui QING Hairuo LIU Qi-guo | 2012 | Journal of Hydrodynamics2012，24，4： | 9 |
| 13 | 川东北地区三叠系飞仙关组白云化流体温度显示文摘根据川东北地区三叠系飞仙关组白云岩的流体包裹体均一温度、氧同位素组成及其温度计算等分析结果,结合典型钻井的埋藏史与热史重建,可以认为川东北地区三叠系飞仙关组大多数白云岩是低温白云化流体作用的结果,只有少数白云岩(白云石)是高温白云化流体作用的结果,低温白云化流体作用的结束深度大约对应着1000~2500m,结束时间大约对应着中三叠世早中期至晚三叠世早中期,高温白云化流体作用的主要深度大约对应着3200—4500m、主要时间大约对应着中侏罗世早中期.低温白云化流体和高温白云化流体对飞仙关组白云岩储集空间的形成与演化有着不同的意义. | 胡作维 黄思静 李志明 Hairuo QING 范明 兰叶芳 | 2012 | 中国科学:地球科学2012，42，12： | 9 |
| 14 | 塔里木盆地塔北、塔中地区寒武系—奥陶系碳酸盐岩中鞍形白云石胶结物特征显示文摘通过对塔里木盆地中、北部地区寒武系—奥陶系碳酸盐岩的研究,发现鞍形白云石胶结物发育比较普遍,常见于孔洞或裂缝之中,乳白色,晶体粗大,晶面弯曲或呈阶梯状,镜下波状消光,晶体内部常见微裂缝,常与热液矿物共生。本文对28个鞍形白云石样品进行了碳、氧、锶同位素测试,结果显示鞍形白云石的δ^(13)C和δ^(18)O值分别介于-2.446‰~0.686‰和-9.101‰~-5.117‰之间,^(87)Sr/^(86)Sr值介于0.708 6~0.710 2之间;流体包裹体测温分析表明,鞍形白云石中气—液两相包裹体的均一温度(T_h)介于121~159.5℃之间,但集中分布在135~145℃之间;根据最后冰融点温度(T_m)求得的白云岩化流体盐度介于21.3%~23.1%之间。这些数据表明,该类型白云石形成于热卤水(盐度是海水的5~8倍)之中。塔里木盆地鞍形白云石与世界范围内其它盆地的鞍形白云石的碳、氧同位素特征基本相似,但其^(87)Sr/^(86)Sr值相对偏低。导致这一现象的原因可能是鞍形白云石形成于来自深部的岩浆热液流体之中,这些流体伴随岩浆侵位或通过切穿基底的深大断裂及其与之相连的次级断裂系统从深部直接进入碳酸盐岩地层中,未经过碎屑岩输导层的长时间运移,所以导致其中形成的鞍形白云石^(87)Sr/^(86)Sr值偏低。 | 王丹 王旭 陈代钊 杨长春 Hairuo Qing 吴茂炳 邢秀娟 | 2010 | 地质科学2010，45，2： | 7 |
| 15 | Evolution and global correlation for strontium isotopic composition of marine Triassic from Huaying Mountains,eastern Sichuan,China显示文摘Strontium isotope stratigraphy (SIS) has progressively become an efficient chemostratigraphic tool in the research and correlation of global geological events, such as global sea level fluctuations, orogeny, and paleoclimatic and paleoenvironmental changes. In this paper, 87Sr/86Sr ratios of the Triassic marine carbonate rock samples from Huaying Mountains, eastern Sichuan are measured, and the corre-sponding Sr-isotopic curve is constructed, based on the fundamental principle of strontium isotope stratigraphy, analysis of rock fabric, luminescent intensity, chemical composition and representative evaluation for the coeval seawater information. The 87Sr/86Sr ratios show a rapid rise from 0.70721 near the Permian-Triassic transition to 0.70830 at the end of Early Triassic, and then they decline rapidly to 0.70787 in the early Middle Triassic. These data are generally coincident with 87Sr/86Sr ratios of coeval seawater from previous papers, and the curve is also similar to other previous curves. This indicates that the global geological events are the most important controlling factors to the strontium isotope evolution of the global seawater in the Early and Middle Triassic. | ZuoWei Hu SiJing Huang HaiRuo Qing QingDong Wang ChunMei Wang XiaoYong Gao | 2008 | Science China Earth Sciences2008，51，4： | 5 |
| 16 | Hydrodynamic analysis of clastic injection and hydraulic fracturing structures in the Jinding Zn-Pb deposit,Yunnan,China显示文摘Jinding Zn-Pb 存款通常被考虑了以一个相对被动的方法从传播 basinal 液体形成了,与液体流动被结构和沉积外形正在控制,类似于许多另外的招待沉积的底金属存款。然而,几最近的研究在 Jinding 存款的开的坑揭示了沙注射结构,恼人的角砾岩,和水力的破裂的存在并且建议存款从 overpressured 液体的爆炸版本被形成。这研究报导液体的新观察过压相关从地下的活动方式(Paomaping 和 Fengzishan ) 组织,它比在开的坑显示出更清楚的横切的关系。观察结构包括:1 ) 沙(楳湧晩捩湡汴 ? 潣瑮楲畢整琠? 桴 ? 潴慴? 票牤 ' 夷典? | Guoxiang Chi Chunji Xue Hairuo Qing Wei Xue Jiangwei Zhang Yunqiang Sun | 2012 | Geoscience Frontiers2012，3，1： | 5 |
| 17 | Characteristics and Dolomitization of Upper Cambrian to Lower Ordovician Dolomite from Outcrop in Keping Uplift, Western Tarim Basin, Northwest China显示文摘Late Cambrian to Early Ordovician sedimentary rocks in the western Tarim Basin, Northwest China, are composed of shallow-marine platform carbonates. The Keping Uplift is located in the northwest region of this basin. On the basis of petrographic and geochemical features, four matrix replacement dolomites and one type of cement dolomite are identified. Matrix replacement dolomites include (1) micritic dolomites (MD1); (2) fine-coarse euhedral floating dolomites (MD2); (3) fine-coarse euhedral dolomites (MD3); and (4) medium-very coarse anhedral mosaic dolomites (MD4). Dolomite cement occurs in minor amounts as coarse saddle dolomite cement (CD1) that mostly fills vugs and fractures in the matrix dolomites. These matrix dolomites have δ18O values of ?9.7‰ to ?3.0‰ VPDB (Vienna Pee Dee Belemnite); δ13C values of ?0.8‰ to 3.5‰ VPDB; 87Sr/86Sr ratios of 0.708516 to 0.709643; Sr concentrations of 50 to 257 ppm; Fe contents of 425 to 16878 ppm; and Mn contents of 28 to 144 ppm. Petrographic and geochemical data suggest that the matrix replacement dolomites were likely formed by normal and evaporative seawater in early stages prior to chemical compaction at shallow burial depths. Compared with matrix dolomites, dolomite cement yields lower δ18O values (?12.9‰ to ?9.1‰ VPDB); slightly lower δ13C values (?1.6‰-0.6‰ VPDB); higher 87Sr/86Sr ratios (0.709165-0.709764); and high homogenization temperature (Th) values (98°C-225°C) and salinities (6 wt%-24 wt% NaCl equivalent). Limited data from dolomite cement shows a low Sr concentration (58.6 ppm) and high Fe and Mn contents (1233 and 1250 ppm, respectively). These data imply that the dolomite cement precipitated from higher temperature hydrothermal salinity fluids. These fluids could be related to widespread igneous activities in the Tarim Basin occurring during Permian time when the host dolostones were deeply buried. Faults likely acted as important conduits that channeled dolomitizing fluids from the underlying strata into the basal carbonates, leading to intense dolomitization. Therefore, dolomitization, in the Keping Uplift area is likely related to evaporated seawater via seepage reflux in addition to burial processes and hydrothermal fluids. | JI Congwei QING Hairuo CHEN Daizhao LUO Ping JIN Zhijun SHAO Longyi | 2013 | Acta Geologica Sinica(English Edition)2013，87，4： | 4 |
| 18 | Temperatures of dolomitizing fluids in the Feixianguan Formation from the Northeastern Sichuan Basin显示文摘The discovery of natural gas reservoirs from the Triassic Feixianguan Formation in the Northeastern Sichuan Basin is an important breakthrough in the field of marine carbonate rocks for Chinese oil and gas exploration in recent years.Because of the dolomite-hosted reservoirs in the Feixianguan Formation,these dolomites and their formation mechanisms have been a research focus for sedimentary geologists and petroleum geologists.Based on the homogenization temperatures of fluid inclusions,oxygen isotopic composition and their calculated temperatures,and the burial and thermal history of the typical well,it is considered that the majority of dolomites are formed by low-temperature dolomitizing fluids in the Triassic Feixianguan Formation,Northeastern Sichuan Basin.Only a minority of dolomites are formed by high-temperature dolomitizing fluids.The ending depth interval of low-temperature dolomitizing fluids was about 1000-2500 m,of which the correspondingly ending timing interval was approximately from early-middle Middle Triassic to early-middle Late Triassic.The main depth interval of high-temperature dolomitizing fluids was about 3200-4500 m,of which the correspondingly main timing interval was approximately early-middle Middle Jurassic.The low-temperature and high-temperature dolomitizing fluids have different meanings to the formation and evolution of the pore volumes of dolomite reservoirs in the Feixianguan Formation,Northeastern Sichuan Basin. | HU ZuoWei HUANG SiJing LI ZhiMing QING HaiRuo FAN Ming LAN YeFang | 2012 | Science China Earth Sciences2012，55，10： | 4 |
| 19 | 青西凹陷下沟组湖相热水沉积岩中的重晶石流体包裹体特征显示文摘以地质背景和岩石组构分析为基础,对酒泉盆地青西凹陷下沟组湖相热水沉积岩中的重晶石矿物进行了流体包裹体研究。结果表明,重晶石胶结物中主要发育富液两相、含子矿物三相、单一液相和单一气相四类原生流体包裹体,碎屑状重晶石主要发育富液两相和少量单一液相包裹体。显微测温结果显示,重晶石胶结物和碎屑状重晶石的成矿流体为NaCl-H2O体系,温度分别为160-200℃和120~140℃,盐度(NaCl)分别为20%~22%和18%~20%,密度分别为1.06~1.2g/cm3和1.06~1.11g/cm3,成矿压力分别为150~180MPa和30~45MPa。结合锶同位素分析,认为成矿流体属于深循环的下渗湖水与岩浆水共同构成的中低温、中高盐度和中偏高密度混合热卤水。成矿流体经历了早期阶段的热液沸腾作用和混合作用的叠加耦合而形成重晶石胶结物,较晚期阶段热液混合稀释沉淀作用则形成碎屑状重晶石。两者应属于同一热流体不同阶段和不同方式的化学沉淀产物,重晶石胶结物形成于喷流口内;碎屑状重晶石形成于相对远离喷流口的开放系统,有更多大气水(湖水)的注入而使得其热流体温度、盐度、密度和压力相比重晶石胶结物均有所下降。重晶石矿物流体特征和成因研究,可为研究区下沟组湖相热水沉积岩热流体性质、来源和成因分析奠定基础。 | 文华国 郑荣才 Hairuo QING 范铭涛 吴国瑄 夏佩芬 汪满福 桑廷元 廖一 陈浩如 | 2008 | 成都理工大学学报(自然科学版)2008，35，3： | 3 |
| 20 | 加拿大西部盆地沉积Presqu'ile障壁岛粗晶热液白云岩储层的成因显示文摘中泥盆统由西南部Pine Point延伸至不列颠哥伦比亚东北山麓之下的Presqu′ile障壁岛的中、晚期粗晶交代白云石伴随着异形白云石胶结物形成了一个广泛分布的成岩相带,分布在加拿大本土的西北部和不列颠哥伦比亚东北地区以及在Pine Point地区的密西西比型矿床的围岩层中,这些白云石构成了烃类储层,反之则为致密灰岩。粗晶交代白云石和异形白云石胶结物是在埋藏过程中形成的,因为它们交代了块状亮晶方解石胶结物,并且连续穿过Watt山组不整合面、晚期缝合线和早期交代白云石以及叠加在硫化物的结晶之后,交代和异形白云石的δ^(18)O值沿Presqu′ile障壁岛上倾方向向东增加,在不列颠哥伦比亚东北部的地下深处为—16‰PDB,在Pine Point为—7‰PDB,而异形白云石流体包裹体的相应均一温度由178℃变化到92℃。粗晶和异形白云石的^(87)Sr/^(86)Sr值沿Presgu′ile障壁岛向东由不列颠哥伦比亚东北部地下的0.7106降低到Pine Point地区的0.7081,这些地球化学趋势表明了热液,放射性成因的白云石化流体向东沿Presqu′ile障壁岛上倾方向在盆地范围内迁移的可能性。如此大规模流体运动很可能与加拿大西部沉积盆地的构造挤压和沉积负载有关,这种运动至少有两期:在晚泥盆和早石炭世时期的早期埋藏期间和晚休罗和早第三世时期? | Hairuo Qing 邓礼正 张子枢 张哨楠 | 1995 | 天然气勘探与开发1995，0，2： | 2 |
您所在的机构暂未开通此部分的功能，请联系管理员