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Uludağ Extensional Metamorphic Core Complex: Preliminary Field Observations Uludağ伸展变质核杂岩:初步野外观测
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-11-27 DOI: 10.19111/bulletinofmre.1029034
G. Seyitoğlu, Korhan Esat
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引用次数: 5
Assessment of Crustal Thinning and Tectonic Stress Distribution of Gülbahçe Fault Zone and Its Surroundings (İzmir, West Turkey) Using Gravity and Magnetic Anomalies 利用重磁异常评价土耳其西部g<s:1> lbahe断裂带及其周围(İzmir)地壳减薄及构造应力分布
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-11-27 DOI: 10.19111/bulletinofmre.1029265
O. Pamukçu, Ayça Çırmık, F. Doğru, Ece Ünlü, Barış Can Malaliçi
Gülbahçe Fault Zone (GFZ) is a significant tectonic structure and seismic source for İzmir city and its surroundings. The major earthquakes occurred at the surroundings of GFZ are 2005 Seferihisar, 2020 Samos Island-Aegean Sea and 2021 Seferihisar earthquakes. In this study, the crustal thinning and tectonic stress distribution of GFZ and its surroundings were analyzed by using the new gravity and magnetic data. The correspondence analysis was applied by appraising together the magnetic and free-air anomaly data. Moreover, the average density of the subsurface structure was calculated by applying the Parasnis method. The deviatoric stress calculation was executed and the change of the physical properties that controls the gravity and magnetic anomaly of the crustal structure of the GFZ and its surroundings from north to south was investigated. Therefore, the average density values, which were obtained from gravity anomalies, were computed as 2.59 gr / cm 3 in the north of the study region and it decreased to 2.06, 1.8 and 1.49 gr / cm 3 towards to the south. The free-air gravity anomaly values were between 0-70 mGal and the magnetic anomalies were between -450-150 nT. The deviatoric stress
Gülbahçe断层带(GFZ)是伊兹密尔市及其周边地区的重要构造和震源。GFZ周围发生的主要地震有2005年塞费里希萨尔地震、2020年爱琴海萨摩斯岛地震和2021年塞费里希萨尔地震。利用新的重磁资料,分析了GFZ及其周围地区的地壳减薄和构造应力分布。应用对应分析法对地磁和自由空气异常资料进行了综合评价。此外,应用Parasnis方法计算了地下结构的平均密度。进行了偏应力计算,研究了控制GFZ及其周围地壳结构重磁异常的物理性质从北到南的变化。因此,从重力异常中获得的平均密度值在研究区域的北部被计算为2.59 gr/cm3,而在南部则分别降至2.06、1.8和1.49 gr/cm 3。自由空气重力异常值在0-70mGal之间,磁异常值在-450-150nT之间
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引用次数: 0
Analysis of the Stress Distribution of North Anatolian Fault Zone for the Part Between Amasya-Tokat Cities 北安纳托利亚断裂带阿玛西亚-托卡特城市间部分应力分布分析
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-11-11 DOI: 10.19111/bulletinofmre.1022323
Ayça Çırmık, U. Aydın, O. Pamukçu, F. Doğru
Tectonic forces formed in the continental crust, cause permanent changes in stress, compression and deformation. The amplitudes of earthquake waves vary with the stress / strain distribution in the crust. In this study, the change of stress / strain and regional absorption coefficient, which is effective in tectonic forces caused by elastic deformation energy accumulating in the brittle crust over time, was investigated. The study area is the middle part of the North Anatolian Fault Zone and the area formed by Ezinepazarı fault zone and Merzifon fault zone. In this area, Coulomb stress analysis was carried out by using the focal mechanism solution values of the earthquake that occurred in Yoldere Erbaa, Tokat on October 9, 2015 (ML = 5.1). In order to examine the deformation caused by this earthquake in and around the study area, Global Navigation Satellite System (GNSS) data were evaluated and the velocities of these stations were calculated using GNSS data of these stations for the years 2013 2014 2015 2016. Also, regional absorption coefficients were determined by using earthquake data. As a result, Coulomb stress analysis results, velocity values distribution obtained from GNSS data and absorption findings obtained from seismological study were evaluated together. Atıf bilgisi: Çırmık, A., Aydın, U., Pamukçu, O.A., Doğru, F. 2022. Analysis of the stress distribution of North Anatolian Fault Zone for the part between Amasya Tokat cities. Bulletin of the Mineral Research and Exploration xxx, x-x. DOI: https://doi.org/10.19111/bulletinofmre.1022323 *Başvurulacak yazar: Ayça ÇIRMIK, ayca.cirmik@deu.edu.tr Maden Tetkik ve Arama Dergisi http://dergi.mta.gov.tr MTA Dergisi (2022) xxx:xx
构造力在大陆地壳中形成,引起应力、压缩和变形的永久性变化。地震波的振幅随地壳中的应力/应变分布而变化。在这项研究中,研究了应力/应变和区域吸收系数的变化,这在脆性地壳中弹性变形能量积累引起的构造力中是有效的。研究区位于北安那托利亚断层带的中部,由Ezinepazarı断层带和Merzifon断层带组成。在该区域,利用2015年10月9日发生在托卡特州约尔德-埃尔巴的地震(ML=5.1)的震源机制解数值进行了库仑应力分析,评估了全球导航卫星系统(GNSS)数据,并使用这些台站2013年、2014年、2015年、2016年的GNSS数据计算了这些台站的速度。此外,还利用地震资料确定了区域吸收系数。结果,库仑应力分析结果、从GNSS数据中获得的速度值分布和从地震学研究中获得的吸收结果被一起评估。地址:Çırmık,A.,Aydın,U.,PamukçU,O.A.,Doğru,f.2022。Amasya-Tokat城市之间的北安那托利亚断层带应力分布分析。矿产研究与勘探公报xxx,x-x。DOI:https://doi.org/10.19111/bulletinofmre.1022323*Başvurulacak yazar:AyçaÇIRMIK,ayca.cirmik@deu.edu.trMaden Tetkik ve Arama Dergisihttp://dergi.mta.gov.trMTA Dergisi(2022)xxx:xx
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引用次数: 0
Extraction of Rubidium Element from Malatya - Kuluncak Area Complex Ore 马拉提亚-库仑卡克地区杂矿石中铷元素的提取
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-09-18 DOI: 10.19111/bulletinofmre.997306
Ayşe Erdem, Hüseyin Eren Obuz, Haydar Güneş, Şölen Di̇ktepe, Buse Ozen Ilik, Çiğdem Kara, H. Akçay, Akan Gülmez, Zümrüt Alkan
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引用次数: 0
Separation Efficiency of Different Methods to Treatment of a Low-Grade Iron Ore 低品位铁矿石不同处理方法的分离效率
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-09-07 DOI: 10.19111/bulletinofmre.992412
Ö. Özcan
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引用次数: 0
Coulomb Stress Change and Size-Frequency Distribution for Lake Van Region 范湖地区库仑应力变化及尺寸-频率分布
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-09-03 DOI: 10.19111/bulletinofmre.990666
H. Alkan, E. Bayrak
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引用次数: 3
A new paradigm for the future of archaeometallurgy in Anatolia: Review of Thai archaeology monograph series (TAM) 安纳托利亚考古冶金未来的新范式——泰国考古专著系列(TAM)述评
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-09-02 DOI: 10.19111/bulletinofmre.990063
G. Dardeniz
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引用次数: 0
Modeling of the complex hydrocarbon traps by the shot domain acoustic finite difference method and data-processing 复杂油气藏的声发射域有限差分建模及数据处理
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-08-20 DOI: 10.19111/bulletinofmre.985502
Şerife Boğazkesen, H. Karslı
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引用次数: 0
Active tectonics of Gülpınar-Tuzla area (Biga Peninsula, NW Turkey): The source of 6 February-24 March 2017 earthquake cluster Gülpınar Tuzla地区(土耳其西北部比加半岛)的活动构造:2017年2月6日至3月24日地震群的来源
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-08-19 DOI: 10.19111/bulletinofmre.984922
A. Koçyi̇ği̇t, Şule Gürboğa
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引用次数: 2
A Walkaway Vertical Seismic Profiling Modeling and Imaging Study and Combining Its Results with Migrated Surface Seismic Images 步行式垂直地震剖面建模与成像研究及其与迁移地表地震图像的结合
IF 0.5 Q3 Earth and Planetary Sciences Pub Date : 2021-08-12 DOI: 10.19111/bulletinofmre.981941
C. Erdemir
This paper presents and analyzes results from a Finite Difference Modeling (FDM), processing, and imaging study of a Walkaway Vertical Seismic Profiling (WVSP) survey, and discusses how the images from WVSP enhance those from the surface seismic data. It is shown that the results from the WVSP integrate well with the image from the surface seismic performed in the same line. For the study, a seismic model with vertically and horizontally varying velocities was built and a WVSP data set was generated. The surface seismic had difficulty showing clear images from the layers with steep dips and near vertical displacements on the model due to the lack of ray coverage. The study demonstrates that the WVSP geometry can record reflections from near vertical layers facing the borehole, which help with imaging the parts of the subsurface structure which were missing in the surface seismic. With the proper combination of the images from the WVSP and the surface seismic, a more complete image profile of the subsurface can be constructed around the borehole. However, while contributing to surface seismic, it is also seen that the WVSP introduces more migration artifacts related to source interval distance and interbed multiples than the surface seismic data.
本文介绍并分析了Walkaway垂直地震剖面(WVSP)测量的有限差分建模(FDM)、处理和成像研究的结果,并讨论了WVSP的图像如何增强地表地震数据的图像。结果表明,WVSP的结果与同一直线上进行的地面地震的图像很好地结合在一起。为了进行研究,建立了具有垂直和水平变化速度的地震模型,并生成了WVSP数据集。由于缺乏射线覆盖,地面地震很难在模型上显示出陡倾角和近垂直位移层的清晰图像。该研究表明,WVSP几何结构可以记录面对钻孔的近垂直层的反射,这有助于对地表地震中缺失的地下结构部分进行成像。通过WVSP和地面地震图像的适当组合,可以在钻孔周围构建更完整的地下图像剖面。然而,在对地表地震有贡献的同时,也可以看出,与地表地震数据相比,WVSP引入了更多与源层距离和互层倍数有关的偏移伪影。
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引用次数: 1
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