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Walkaway Vertical Seismic Profiling (WVSP) Modeling and Imaging Study along FaultedCoal Seams over a High Velocity Limestone Model: A Synthetic Study 高速石灰岩模型上沿断层煤层的Walkaway垂直地震剖面(WVSP)建模与成像研究:一项综合研究
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1776
C. Erdemir
: The problem of collecting reflection data from the layers below a high velocity layer (HVL) and imaging those layers accurately is solved using walkaway vertical seismic profiling (WVSP) technique. The procedure is shown on a dataset from a model of highly faulted, thin-bedded coal layers separated by a high velocity layer of limestone. By locating the receivers above, in, and below the HVL, the reflections are expected to be recorded locally in situ in the borehole below the HVL before they travel back to the surface as in the case of surface seismic. The imaging results obtained from the model (or synthetic) WVSP data lead to the conclusion that promising results may be obtained via the acquisition of field WVSP data such that the layers below the HVL are well-imaged. Analysis of the test results showed that the layers below the HVL can be imaged accurately and robustly when the receivers are situated below the HVL only, while the strong images below the HVL tend to fade away and lose their strength when the receivers are moved above the HVL. However, both these cases of the receiver location geometry are needed to obtain images that are vertically and horizontally stable. When a full instrumentation of the borehole is provided, good images as far as 500 m away from the VSP borehole are obtained from the layers with various dips and faults that are nearly 800 m in depth from the surface. Two cases of velocities (4000 m/s and 5000 m/s) are tested for the high velocity limestone layer. Both cases showed good images below the HVL. Unfortunately, some pulled-up effects are seen in the images right below the HVL where the layers that are immediately below the HVL are imaged above their correct locations, the pulled-up effects are corrected in the deeper sections below the HVL however.
:使用步行垂直地震剖面(WVSP)技术解决了从高速层(HVL)以下的层收集反射数据并对这些层进行精确成像的问题。该程序显示在一个由高速石灰岩层分隔的高度断层薄层煤层模型的数据集上。通过将接收器定位在HVL之上、之中和之下,在反射返回地表之前,预计反射将在HVL之下的钻孔中就地记录,就像在地表地震的情况下一样。从模型(或合成)WVSP数据获得的成像结果导致这样的结论,即通过采集场WVSP数据可以获得有希望的结果,使得HVL下方的层被良好地成像。对测试结果的分析表明,当接收器仅位于HVL下方时,HVL下方的层可以准确而稳健地成像,而当接收器移动到HVL上方时,HVL下方的强图像往往会逐渐消失并失去强度。然而,接收器位置几何形状的这两种情况都需要获得垂直和水平稳定的图像。当提供完整的钻孔仪器时,从距离地表近800米深的具有各种倾角和断层的地层中,可以获得距离VSP钻孔500米的良好图像。针对高速石灰岩层测试了两种速度情况(4000m/s和5000m/s)。两例均显示HVL以下图像良好。不幸的是,在HVL正下方的图像中可以看到一些上拉效应,其中直接位于HVL下方的层在其正确位置上方成像,然而,上拉效应在HVL下方较深的部分中被校正。
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引用次数: 0
Further contribution to the early Miocene woody flora of Galatian Volcanic Provincefrom Doğanyurt Village, Ankara (Turkey) 来自Doğanyurt Village, Ankara (Turkey)对加拉太火山省早中新世木本植物群的进一步贡献
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1763
Ü. Akkemik, Stănilă Iamandei, H. Çelik
time in Turkey. Abstract: The Galatian Volcanic Province (GVP) located in central-north Anatolia had a rich woody flora. The purpose of the present study is to contribute to the early Miocene woody flora of the GVP from two fossil sites from Doğanyurt Village of the city of Beypazarı in the Province of Ankara. The fossil sites, which are near to each other, have small pieces of fossil woods. Total 16 fossil woods were collected from two neighbour sites. Three thin sections as transversal, tangential and radial sections from each sample were taken, and they were identified microscopically. As a result, ten fossil species were identified, three of which are new ( Cercioxylon mediterraneum Akkemik, Iamandei & Çelik, sp. nov., Cryptocaryoxylon irregularis Akkemik, Iamandei & Çelik, sp. nov., and Myricoxylon doganyurtensis Akkemik, Iamandei & Çelik sp. nov.) and the rest fossil species ( Glyptostroboxylon rudolphii Dolezych & van der Burgh, Taxodioxylon gypsaceum (Göppert) Kräusel, Pinuxylon Gothan, Aceroxylon aceroides Akkemik, Pistacioxylon ufukii Akkemik, Salicoxylon galatianum Akkemik, and Ulmoxylon cf. carpinifolia Greguss ) are found also in these two fossil sites. The fossil Myrica, identified for the first time in Turkey as a wood, has many leaf fossils from the early Miocene sites. The most common fossil trees in the Miocene time of GVP, which are G. rudolphii and T. gypsaceum , were also identified in these new sites. The fossil wood assemblage may indicate that the area had a subtropical climate in lowland, with riparian and
时间在土耳其。摘要:加拉太火山省(Galatian Volcanic Province, GVP)位于安纳托利亚中北部,具有丰富的木本植物群。本研究的目的是通过安卡拉省贝帕扎尔林Doğanyurt村的两个化石遗址,为GVP早中新世木本植物区系做出贡献。化石遗址彼此靠近,有小块的树木化石。在两个相邻的地点共收集了16块化石木材。从每个样品上取横向、切向和径向三个薄片,并在显微镜下进行鉴定。结果共鉴定出10个化石种,其中3个为新化石种(地中海Cercioxylon Akkemik, Iamandei & Çelik, sp. nov., Cryptocaryoxylon irregularis Akkemik, Iamandei & Çelik, sp. nov.,和Myricoxylon doganyurtensis Akkemik, Iamandei & Çelik sp. nov.),其余化石种(Glyptostroboxylon rudolphii Dolezych & van der Burgh, Taxodioxylon gypsaceum (Göppert) Kräusel, Pinuxylon Gothan, Aceroxylon aceroides Akkemik, Pistacioxylon ufukii Akkemik,在这两个化石地点也发现了Salicoxylon galatianum Akkemik和Ulmoxylon cfr . carpinifolia Greguss。在土耳其首次发现的杨梅化石是一种木材,它有许多来自中新世早期遗址的叶子化石。在这些新址上还发现了GVP中新世最常见的化石树G. rudolphii和T. gypsaceum。化石木材组合可能表明该地区为亚热带低地气候,以河岸和河岸为主
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引用次数: 1
Geochemical and petrographic approach for the origin of the limestone blocks of thewalls of the Great Temple of Hattusha, Çorum (N-Turkey) 哈图沙大神庙石墙石灰岩块的地球化学和岩石学研究,Çorum (n -土耳其)
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1774
İ. Yılmaz, A. Schachner, I. Uysal, Ezgi Ünal İmer
: The socle stones of the Great Temple in the Lower City of the Hittite capital city, Hattusha (Çorum Province) have been studied for the first time by petrographic and geochemical analysis (Sr isotope, stable isotope, and trace element geochemistry). Study objectives were to determine the carbonate facies of the stone samples used in the Great Temple and investigate their possible sources. Petrographic analysis of 10 limestone samples presents five clusters of different microfacies. Stable isotope (δ 13 C and δ 18 O) analysis displayed the presence of 5 groups in parallel with petrographic analysis. Trace element analysis of the same groups displayed considerable difference among the stone samples and 87 Sr/ 86 Sr isotope ratios change between 0.70697 and 0.706867. Based on the results, it can be stated that the building using stones are from probably five different sources. This is of great importance to better understand the construction process and the acquisition of the building materials.
:首次通过岩石相学和地球化学分析(Sr同位素、稳定同位素和微量元素地球化学)对赫梯首都哈图沙下城(Çorum省)的大庙的基石进行了研究。研究目的是确定大庙中使用的石头样品的碳酸盐相,并调查其可能的来源。对10个石灰岩样品的岩石学分析表明,存在5组不同的微相。稳定同位素(δ13C和δ18O)分析显示,在岩相分析的同时,存在5组。同一组的微量元素分析显示,石头样本之间存在相当大的差异,87Sr/86Sr同位素比率在0.70697和0.706867之间变化。根据这些结果,可以说使用石头的建筑可能来自五个不同的来源。这对于更好地了解建筑材料的施工过程和获取具有重要意义。
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引用次数: 0
Reducing uncertainty with fault seal analysis: A case study of Jherruck Block, LowerIndus Basin, Pakistan 通过断层封闭性分析减少不确定性:以巴基斯坦下印度河盆地Jherruck区块为例
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1775
Mudassar Nawaz, Muhammad Rustam Khan, U. Nisar, M. R. Mughal
: Faults can be either conduits or baffles for hydrocarbon flow. Assessing the sealing potential of faults plays a vital role in reducing the risks associated with hydrocarbon exploration. The study area is located in Jherruck Block, Lower Indus Basin, Pakistan. Several intervals within the Lower Goru Formation in Lower Indus Basin are proven hydrocarbon reservoirs. The main aim of the study is to predict the cause of failure of 3 wells (Jherruck B-1, Jamali-1, and Jamali Deep-1), and to propose a new well location based on juxtaposition analysis and shale gouge ratio (SGR). The Upper Sands (sandstone) of the Lower Goru Formation (A-Sand, B-Sand, C-Sand, and D-Sand) have reservoir potential in the region including the Jherruck Block. These reservoir sands have been interpreted in seismic sections to generate time and depth surface maps. Using depth surface maps, Allan diagrams have been constructed for juxtaposition and shale gouge ratio analysis. The integration between juxtaposition and shale gouge ratio analysis suggested that the main reason for the failure of these wells was sandstone to sandstone juxtapositions leading to updip hydrocarbon leakage to the adjacent fault block. In addition to this, the shale gouge ratio indicated low shale gouge distribution in the fault zones. Allan diagram and shale gouge ratio analyses helped us to propose a new well location further northwest of Jherruck B-1 well where sands are juxtaposed against impermeable shale lithology of the Goru Formation and SGR ratio is above 80%
断层既可以是油气流动的管道,也可以是油气流动的屏障。评估断层的封闭潜力对降低油气勘探风险起着至关重要的作用。研究区位于巴基斯坦下印度河盆地Jherruck区块。下印度河盆地下Goru组的几个层段已被证实为油气储层。研究的主要目的是预测3口井(Jherruck B-1、Jamali-1和Jamali Deep-1)的失效原因,并基于并置分析和页岩泥比(SGR)提出新的井位。在包括Jherruck地块在内的该地区,下Goru组的上砂(砂岩)(a砂、b砂、c砂和d砂)具有储集潜力。这些储层砂已经在地震剖面中进行了解释,以生成时间和深度表面图。利用深度表面图,Allan图已被构建用于并置和页岩泥比分析。并置与泥泥比综合分析表明,砂岩与砂岩并置导致油气上倾渗漏至邻近断块是导致这些井失败的主要原因。此外,页岩泥比值表明断裂带内页岩泥分布较低。Allan图和页岩泥比分析帮助我们在Jherruck B-1井的西北方向提出了一个新的井位,在那里,砂岩与Goru组的不渗透页岩岩性并列,SGR比超过80%
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引用次数: 0
Holocene sedimentary history of South Danamandıra Lake: a peatland in west of İstanbul, Çatalca Peninsula, NW Turkey 南达纳曼德拉湖全新世沉积史:土耳其西北部恰塔尔卡半岛伊斯坦布尔西部的泥炭地
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1809
Özlem Makaroğlu, Melda Küçükdemirci, Nurgül Karlıoğlu, Dursun Acar, A. Gürel, R. Dağdeviren, N. Yakupoğlu, Asen Sabuncu, Damla Şahi̇n Altun, M. Karaöz, M. N. Çağatay
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引用次数: 0
Tectonomagmatic reconstruction of the Upper Mesozoic-Cenozoic Neotethyan arcs in the Lut block, East Iran: a review and synthesis 伊朗东部鲁特地块上中生代-新生代新特提斯弧的构造岩浆重建:综述与综合
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1818
R. Arjmandzadeh, S. Alirezaei, Alireza Almasi
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引用次数: 0
Mineralogical and geochemical signatures of weathering on carbonate rocks and dynamic young land surfaces in Muğla Polje (SW Turkey) Muğla Polje(土耳其西南部)碳酸盐岩和动态年轻地表风化的矿物学和地球化学特征
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1820
Ceren Küçükuysal, M. Gül, Tural Aghayev, Merve Gülcan
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引用次数: 0
Detrital composition of Triassic to Neogene sandstones in the Sulaiman Fold-Thrust Belt, Pakistan: implications for pre- and postcollisional evolution of the northwestern Indian margin 巴基斯坦苏莱曼褶皱冲断带三叠纪至新近系砂岩的碎屑组成:对印度西北边缘碰撞前后演化的影响
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1807
Shazia Fareed, A. Kassi, A. Kasi, N. Aysal
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引用次数: 0
Growth of the imbrication zone along the southeast Anatolian orogenic belt: evidencefrom fission track thermochronology from Gölbaşı region (SE Turkey) 东南安纳托利亚造山带叠瓦带发育:来自Gölbaşı地区(土耳其东南部)裂变径迹热年代学的证据
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1761
Y. Topak
: One of the major components of continental collision zones is their imbricated zones. Such a zone along the Southeast Anatolian Orogenic Belt (SAOB) is solely controlled by a still-active convergence and accretion system between the Anatolian Plate and Arabian platform since at least Late Cretaceous. The zone is characterized by NEE/SWW-trending, northward-dipping thrust slices that are squeezed between the Tauride Block to the north and the Arabian platform to the south. The units cropping out within the zone comprise Neo-Tethys-related magmatic, ophiolitic, sedimentary and metamorphic rocks with Late Cretaceous to Miocene formation/metamorphism ages. The Karanlıkdere granitoid intrudes into Late Cretaceous Meydan ophiolite, Helete volcanics, and Malatya metamorphics. These units thrust over Cenozoic volcanic and sedimentary rocks. Although various scenarios have been proposed for the late Cretaceous to Neogene evolution of the complex region, quantitative data aiming to understand the growth mechanism of the imbrication zone in the region are limited. The zircon U-Pb and the apatite fission track (AFT) thermochronology were applied to the Karanlıkdere granitoid within the imbrication zone of the Southeast Anatolian Orogenic Belt (SAOB). The LA-ICP-MS zircon U-Pb age yields 79.67 ± 0.24 Ma with 0.23–0.65 Th/U ratios. This age is slightly younger than the previously published ages, indicating that the main body of the Karanlıkdere granitoid formed 3-4 Ma later than the small dikes intruded into other units. The AFT ages are directly controlled by altitude and range between 40.38 ± 3.4 Ma and 22.81 ± 0.63 Ma. The oldest AFT age has the highest altitude, whereas the youngest has the lowest height. The age-temperature models show a slow uplift rate between 40 Ma and 22 Ma. The results indicate that the growth of the imbrication zone in front of the Nappes of the SAOB continued in a steady-state mode with a slow uplift rate of 0.02 ± 0.005 mm/a, during middle-late Eocene to early Miocene and increasing uplift rate during early-middle Miocene, which might be explained by continental collision during early-middle Miocene.
大陆碰撞带的主要组成部分之一是叠瓦构造带。东南安纳托利亚造山带(SAOB)的这一构造带完全受至少晚白垩世以来安纳托利亚板块与阿拉伯地台之间仍然活跃的辐合和吸积系统控制。该带的特征是北东东/西南西向、北倾的逆冲断层,挤压在北部的Tauride地块和南部的阿拉伯地台之间。在该区内出现的单元包括与新特提斯有关的岩浆、蛇绿岩、沉积岩和变质岩,其形成/变质期为晚白垩世至中新世。Karanlıkdere花岗岩类侵入晚白垩世梅丹蛇绿岩、Helete火山岩和Malatya变质岩。这些单位在新生代火山岩和沉积岩上逆冲。尽管对该复杂地区晚白垩世至新近纪的演化提出了多种设想,但旨在了解该地区叠瓦带生长机制的定量数据有限。应用锆石U-Pb和磷灰石裂变径迹(AFT)热年代学对东南安纳托利亚造山带叠瓦带Karanlıkdere花岗岩类进行了研究。LA-ICP-MS锆石U- pb年龄为79.67±0.24 Ma, Th/U比值为0.23 ~ 0.65。这一年龄比前人公布的年龄略小,说明Karanlıkdere花岗岩类主体形成时间比侵入其他单元的小岩脉晚3 ~ 4 Ma。在40.38±3.4 Ma和22.81±0.63 Ma之间,AFT年龄受海拔高度直接控制。年龄最大的AFT年龄高度最高,而年龄最小的AFT年龄高度最低。年龄-温度模式显示在40 ~ 22 Ma之间抬升速率缓慢。结果表明,在始新世中晚期至中新世早期,南洋逆推覆体前叠瓦带以缓慢的隆升速率(0.02±0.005 mm/a)增长,在中新世早期至中中新世早期隆升速率加快,这可能与中新世早期的大陆碰撞有关。
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引用次数: 1
Relative tectonic activity assessment of Kütahya Graben (Western Anatolia): Insights from geomorphic indices 西安纳托利亚k<e:1>塔哈地堑相对构造活动评价:来自地貌指数的启示
IF 1 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-01-01 DOI: 10.55730/1300-0985.1808
Zeynep Kezer, E. Özsayın
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引用次数: 0
期刊
Turkish Journal of Earth Sciences
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