南海北部无明显BSR地区天然气水合物识别研究   总被引：1，自引：0，他引：1  

杨睿  吴能友  白杰  苏正  梁金强  沙志彬 《地球物理学进展》2013,28(2)

似海底反射(BSR)作为海域天然气水合物的重要地震识别标志之一,已得到广泛认同.然而,科学钻探证实,天然气水合物和BSR之间并不具有严格对应关系,即存在水合物的地区却并不一定存在BSR.本文在分析BSR与天然气水合物非充分必要对应关系及其原因的基础上,着重对无明显BSR地区天然气水合物的地震识别方法和应用进行研究.对经钻探证实的存在天然气水合物的神狐海域地震资料进行处理分析后发现,含水合物沉积层具有层速度相对较高、高波阻抗、瞬时高频等特征,且层速度反演、波阻抗反演和瞬时属性分析等方法能有效识别无明显BSR区域的天然气水合物.最后,综合利用这些识别方法,应用于琼东南盆地无明显BSR地区的天然气水合物地震识别,取得了较好的效果.  相似文献   

江苏省地电阻率年变化及其差异性探讨     

沙宏武  龚永俭  孙春仙 《防灾减灾学报》2013,(4):35-39

以江苏省江宁地震台、新沂地震台和海安地震台为例,归纳了江苏省地电阻率年变化特征的类型,并对地电阻率年变化差异性的原因做了探讨。通过反演计算指出地电阻率年变化差异性的原因主要是由各观测场地地下电性结构造成的,分析这种不同有益于解决在场地选择中如何得到一个规则年变的场地,以便更好地服务于地震预报的数据处理。  相似文献   

商河县郑路镇中低产田项目治理综合效益分析     

聂德久  王云祥  刘娟娟  沙福建  王金博 《山东地质》2012,(5):58-59,62

土地整理效益研究是土地整理理论及实践研究的重要组成部分,也是当今土地科学领域专家和学者关注的重要课题。结合商河县郑路镇项目区的自然和社会经济条件以及土地利用状况,对土地开发整理项目进行社会效益、生态效益及经济效益分析,指出土地整理应寻求社会、生态和经济三大效益的最大结合,实现效益最大化,最终促进农村经济的可持续发展。  相似文献   

中国非海相白垩纪介形类化石组合     

王亚琼  沙金庚  泮燕红  张晓林  饶馨 《地层学杂志》2012,(2):289-299

我国非海相白垩纪介形类化石可以划分为7个组合:1)分布于我国西北和西南地区欧特里沃期巴列姆期的Jingguella-Minheella-Pinnocypridea组合;2)分布于我国西北和西南地区巴列姆期的Cypridea-Latonia-Darwinula组合;3)阿普特期阿尔必期的Cypridea(Morinina)-Bisulcocypridea-Mongolocypris组合;4)分布于我国东北、中部及东部地区欧特里沃期巴列姆期的Cypridea-Mongolianella-Darwinula组合;5)分布于我国东北、中部及东部地区巴列姆期阿普特期的Cypridea(Cypridea)-Cypridea(Ulwellia)-Limnocypridea组合;6)塞诺曼期塞农期的Cypridea-Triangulicypris-Sunliavia-Lycopterocypris组合;7)坎潘期马斯特里赫特期的Talicypridea-Cypridea-Quadracypris-Candona组合。依据以上7个介形类化石组合,我国22个地区含介形类的73个地层单元(群/组)得到了对比。  相似文献   

中国东北、韩国东南和日本西南部早白垩世非海相与海相地层对比,非海相软体动物的生物年代学和古地理意义     

沙金庚  泮燕红  王亚琼  张晓林  饶馨 《地层学杂志》2012,(2):357-381

根据非海相与海相,特别是共同的海相和非海相软体动物化石的对比,并结合放射性同位素测年,中国东北黑龙江东部和辽宁西部,韩国东南部庆尚盆地,日本西南部内带岐阜县北部牧户/庄川地区和外带四国德岛和物部地区早白垩世地层得到了对比,产自这些地层的非海相软体动物的时代也因此受到了约束。著名的中国东北含煤地层龙爪沟和鸡西群,盛产热河生物群/动物群的热河群的时代均为欧特里沃期/巴列姆期阿普特期,它们的上覆地层桦山群和孙家湾组为阿尔必期。韩国西南部新洞群和除金洞组以外的河阳群为阿普特期阿尔必期,不整合于新洞群之下的卯谷组主要为欧特里沃期。日本西南部内带的牧户/庄川地区的手取群和外带德岛和物部地区的物部川群均为欧特里沃期阿尔必期。Cuniopsis kihongi,Nakamuranaia leei,Koreanaia cheongi和Trigonioides(Wakinoa)tetoriensis的时代为欧特里沃期早巴列姆期。Viviparus onogoensis,Unio ogamigoensis,Myrene(Mesocorbicular)tetoriensis及Tetoria(Tetoria)yokoyami为欧特里沃期阿普特期。Arguniella cf.quadrata,A.cf.ventricosa,Sphaerium(Sphaerium)anderssoni,Probaicalia vitimensis和Pr.gerassimovi为欧特里沃期/巴列姆期阿普特期。Nakamuranaia chingshanensis,Plicatounio(Plicatounio)multiplicatus,Sphaerium(Sphaerium)coreanicum和Micromelania?katoensis为阿普特期阿尔必期。Nippononaia sinensis,Nip.tetoriensis,Nip.ryosekiana和Trigo-nioides(Wakinoa)wakinoensis是阿普特期的标志。Trigonioides(Trigonioides)quadratus,T.(T.)heilongjiangensis,Plicatounio(Plicatounio)naktongensis,Unio longus与Sphaerium(Sphaerium)chintaoense为晚阿普特期阿尔必期或阿尔必期的标志化石。我国东北、韩国东南和日本西南部非海相,特别是淡水软体动物接近的相似性表明这三地区在早白垩世时相连,并处于同一水系。但是,在欧特里沃期阿尔必期期间,这一陆块的东部,即频临古太平洋的日本西南部的外带因地势低而多被海水覆盖,在牧户/庄川和黑龙江东部存有遭受海侵的浅而窄的海湾,凡兰吟期,特别是欧特里沃期/巴列姆期之前,中国东北韩国东南部日本西南部陆块为受造山运动引起的隆起和沉降活动影响的高低不平的高原,经受了广泛而长期的剥蚀。多数含有包括熔岩和凝灰岩在内的火山岩,并与北东北北东方向的断裂带近于平行分布的非海相白垩纪盆地直至欧特里沃期/早巴列期(有些地区可能稍早(凡兰吟期))(134～126Ma),即华北克拉通破坏的高峰期(130～120Ma)才形成。这一现象表明,这些盆地受断裂,特别是伴随有强烈火山喷发和时而局部海侵的沿着古太平洋西北缘和郯庐断裂带的构造运动的控制。  相似文献   

影响声波全波列测井速度分析的因素剖析     

沙振海 《地质与勘探》2012,48(4):784-789

[摘 要] 目前,速度分析是声波全波列测井提取纵、横波速度的必要流程。本文介绍了井场中的声 波波形成分,提出了一种相似相关速度分析算法,并在其基础上深入研究了影响速度分析结果的关键因 素,如带通滤波,窗口宽度,总叠加时间,以及低速地层等等。通过讨论分析,给出了这些处理参数在速 度分析中的取值,它对精确提取岩石纵、横波速度有着重要的指导意义。  相似文献   

小波阈值消噪方法分析及应用   总被引：1，自引：0，他引：1  

沙磊  任超  彭家頔  文鸿雁 《测绘信息与工程》2011,36(6):15-17

详细介绍了小波阈值消噪中阈值函数的选取和阈值的具体估计方法,并对阈值函数的选取进行了比较分析,以四川二滩大坝变形监测数据消噪前后的信噪比和均方根误差两个指标,对各种阈值方法进行了对比分析。理论分析、应用实例的结果表明,几乎硬阈值方法比Garrote阈值方法能更好地恢复被噪声湮没的局部变形信息。  相似文献   

Stratigraphy of the Triassic?Jurassic Boundary Successions of the Southern Margin of the Junggar Basin, Northwestern China   总被引：2，自引：1，他引：1  

SHA Jingeng  Vivi VAJDA  PAN Yanhong  Linda LARSSON  YAO Xiaogang  ZHANG Xiaolin  WANG Yaqiong  CHENG Xiansheng  JIANG Baoyu  DENG Shenghui  CHEN Siwei  PENG Bo 《《地质学报》英文版》2011,85(2):421-436

The Triassic?Jurassic (Tr?J) boundary marks a major extinction event, which (~200 Ma) resulted in global extinctions of fauna and flora both in the marine and terrestrial realms. There prevail great challenges in determining the exact location of the terrestrial Tr?J boundary, because of endemism of taxa and the scarcity of fossils in terrestrial settings leading to difficulties in linking marine and terrestrial sedimentary successions. Investigation based on palynology and bivalves has been carried out over a 1113 m thick section, which is subdivided into 132 beds, along the Haojiagou valley on the southern margin of the Junggar Basin of the northern Xinjiang, northwestern China. The terrestrial Lower Jurassic is conformably resting on the Upper Triassic strata. The Upper Triassic covers the Huangshanjie Formation overlaid by the Haojiagou Formation, while the Lower Jurassic comprises the Badaowan Formation followed by the Sangonghe Formation. Fifty six pollen and spore taxa and one algal taxon were identified from the sediments. Based on the key-species and abundance of spores and pollen, three zones were erected: the Late Triassic (Rhaetian) Aratrisporites?Alisporites Assemblage, the Early Jurassic (Hettangian) Perinopollenites?Pinuspollenites Assemblage, and the Sinemurian Perinopollenites?Cycadopites Assemblage. The Tr?J boundary is placed between bed 44 and 45 coincident with the boundary between the Haojiagou and Badaowan formations. Beds with Ferganoconcha (?), Unio?Ferganoconcha and Waagenoperna?Yananoconcha bivalve assemblages are recognized. The Ferganoconcha (?) bed is limited to the upper Haojiagou Formation, Unio?Ferganoconcha and Waagenoperna?Yananoconcha assemblages are present in the middle and upper members of the Badaowan Formation. The sedimentary succession is interpreted as terrestrial with two mainly lake deposit intervals within Haojiagou and Badaowan formations, yielding fresh water algae and bivalves. However, the presence of brackish water algae Tasmanites and the marine?littoral facies bivalve Waagenoperna from the Badaowan Formation indicate that the Junggar Basin was influenced by sea water caused by transgressions from the northern Tethys, during the Sinemurian.  相似文献   

Geochemistry of Palaeozoic marine petroleum from the Tarim Basin, NW China: Part 3. Thermal cracking of liquid hydrocarbons and gas washing as the major mechanisms for deep gas condensate accumulations   总被引：2，自引：0，他引：2  

Shuichang Zhang  Jin Su  Xiaomei Wang  Guangyou Zhu  Haijun YangKeyu Liu  Zhenxi Li 《Organic Geochemistry》2011,42(11):1394-1410

The Lunnan Lower Uplift in the Tarim Basin, NW China contains a composite petroleum system with mainly biodegraded heavy oil in the west, normal oil in the center and gas condensate in the east. Twenty-three gas samples and 37 oil samples taken from three major hydrocarbon bearing intervals in the Lunnan lower bulge were analyzed for their stable carbon isotopes and molecular biomarkers. On the basis of their isotopic compositions, biomarkers, especially diamondoids, and integrating the physical properties of the hydrocarbons including densities, GOR and PVT relationships, it has been concluded that the recently discovered deep (6500 m) eastern Lungu giant Ordovician gas condensate pool with an estimated reserve of 723 million bbl oil equivalent is a secondary hydrocarbon accumulation derived from the mixing of an early formed oil and a late formed gas. The extremely dry gases with a gas dryness of >0.98 were derived from thermal cracking of crude oils and charged to an existing oil reservoir causing extensive gas washing and secondary alteration. Compared with most of the hydrocarbons in the Lunnan area, the gas from the eastern Lungu gas condensate pool has a heavier carbon isotopic composition, higher dryness and a higher maturity level. The unique physical, chemical and isotopic compositions of the gas condensate are believed to be a direct result of gas flushing of an early formed eastern Lungu oil pool by a late formed dry gas from oil cracking. The eastern Lungu gas condensate pool is presently characterized by containing “dry gas, heavy oil, abundant aromatics and high wax”.  相似文献   

Heat flow pattern, base of methane hydrates stability zones and BSRs in Shenhu Area, northern South China Sea   总被引：2，自引：2，他引：0  

ZHANG Yi  HE Lijuan  WANG Jiyang  XU Xing  SHA Zhibing  GONG Yuehu  WANG Hongbing  LIANG Jinqiang 《海洋学报(英文版)》2011,30(1):59-67

Using the collected 433 heat flow values, we estimated the bases of methane hydrate stability zone (BHSZ), in northern South China Sea (NSCS). Through comparing BHSZs with the depths of bottom simulating reflectors (BSRs), in Shenhu Area (SA), we found that there are big differences between them. In the north of SA, where the water depth is shallow, many slumps developed and the sedimentation rate is high, it appears great negative difference (as large as -192%). However, to the southeast of SA, where the water depth is deeper, sedimentation rate is relatively low and uplift basement topography exists, it changes to positive difference (as large as +45%). The differences change so great, which haven’t been observed in other places of the world. After considering the errors from the process of heat flow measurement, the BSR depth, the relationship of thermal conductivity with the sediments depth, and the fluid flow activities, we conclude that the difference should be not caused by these errors. Such big disagreement may be due to the misunderstanding of BSR. The deviant “BSRs” could represent the paleo-BSRs or just gas-bearing sediment layers, such as unconformities or the specific strata where have different permeability, which are not hydraterelated BSRs.  相似文献