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A new look at the origin of N-S trending young basins of western Anatolia 对安纳托利亚西部南北走向年轻盆地起源的新认识
IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-02-02 DOI: 10.19111/bulletinofmre.1066949
Ö. F. Gürer
ÖZ Batı Anadolu’da, Geç Senozoyik sırasında kabuk kısalmasından genişlemesine bir geçiş gerçekleşmiş ve bunun kanıtları bölgedeki temel birimlerinde ve K-G ve D-B yönlü, iki farklı havza türünde kaydedilmiştir. Bu çalışmada havzaların tabanında yer alan ve bölgenin yapısal gelişiminde önemli bir rolü olan Menderes Masifi’nin yüzeylenme mekanizması farklı bir açıdan göz önüne alınmıştır. Farklı temeller üzerinde gelişen K-G yönlü havzalar bölgedeki yeni bulgular ışığında değerlendirilmiştir. Elde edilen bulgular bölge üzerinde süre gelen tartışmaları kısıtlayabilecek yeni sonuçlar üretme potansiyelindedir. Gözlemlerimiz ışığında önerilen modele göre, Batı Anadolu Erken-Orta Miyosen sırasında, K-G yönlü sıkışmalı kuvvetler etkisi altındadır. Sıkışma nedeniyle, Menderes Masifi sıkışmalı çekirdek karmaşığı olarak yükselmiş ve yüzeylenmiş olmalıdır. Bu dönemde Marmara’dan Akdeniz’e kadar geniş bir coğrafyada K-G doğrultulu, oblik faylar arasında Gördes ve Demirci gibi çek ayır veya transtansiyonel çek ayır havzalar oluşmuştur. Bölgede Erken-Orta Miyosen’deki yaygın sıkışmanın kanıtları, K-G yönlü havzaları sınırlayan doğrultu atımın egemen olduğu oblik faylar, havza dolgularında gelişen kıvrımlar ve ters faylardır. Sıkışmalı tektonik rejimin, Pliyo-Kuvaterner’de gerilmeli rejime dönüşümü ile tüm bölge K-G yönünde gerilmiş ve bölgenin karakteristik yapısal özelliklerinden olan D-B yönlü Gediz, Büyük Menderes ve Gökova gibi grabenler gelişmiştir. K-G yönlü havzaların aksine, D-B yönlü grabenlerde normal faylar ve yer yer gerilmeyle ilişkili açık kıvrımlar gözlenmektedir. Geç Senozoyik yaşlı havzalardan elde edilen verilere göre bölgede çok evreli gerilmenin izleri gözlenmiştir. Anahtar Kelimeler: Batı Anadolu, Geç Senozoyik, Sıkışmalı tektonik, K-G havzalar, Neotektonik
在西阿纳多卢,在Senozoyic后期,出现了扩大货架短缺的过渡,该地区的主要单位以及两个不同季节的K-G和D-B路线都记录了证据。在本研究中,以不同的方式观察了Menderes-Masifi表面机制,它是该地区建设发展的重要组成部分。该地区的新发现是根据不同场地的K-G方向水池进行评估的。所收到的调查结果有可能限制正在进行的关于该地区的讨论。根据我们的监测提出的模型,在米约森西部阿纳多卢-埃尔肯中部,K-G方向的压缩力受到影响。由于碰撞,Menderes Masiphi必须作为一种复杂的心脏并发症进行饲养。当时,K-G中已经展示了一幅马尔马拉到海洋的大图,画在Görses和Demirci等形状区域之间,或跨大西洋支票之间。Eren Middle Miyosen大范围紧张的证据有助于控制K-G海滩的马匹、海洋填充物和相反的影响。随着Pliyo Kuvaterner斗争政权的转变,斗争的技术政权发展出了Gediz、Great Menderes和Gökova等抓手,这是该地区的特色。与K-G方向的水池不同,D-B方向的抓取器正在寻找与正常文件和地面移除相关的开放曲线。根据从Senozoyic晚期旧水池获得的数据,该地区受到了大量反向张力的监测。关键词:西阿纳多卢、Senozoyic晚期、钻孔构造、K-G油气藏、新构造
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引用次数: 5
Estimation of blast vibrations by numerical modelling and signal analysis 用数值模拟和信号分析估计爆炸振动
IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2022-02-02 DOI: 10.19111/bulletinofmre.1066943
Guzın Gulsev UYAR AKSOY
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引用次数: 0
Gis-based analytical hierarchy process, weight of evidence and logistic regression models for the landslide susceptibility predicting in Echorfa Region (northwestern of Algeria) Echorfa地区(阿尔及利亚西北部)滑坡易发性预测的基于Gis的层次分析法、证据权重和逻辑回归模型
IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2021-12-11 DOI: 10.19111/bulletinofmre.1035480
Roukh ZİNE EL ABİDİNE, Nadjı Abdelmansour
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引用次数: 0
Mordoğan (Karaburun-İzmir) Çevresinin Neojen Stratigrafisi ve Bölgesel Korelasyonu, Batı Anadolu
IF 0.5 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2021-12-11 DOI: 10.19111/bulletinofmre.1035471
Fikret Göktaş
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引用次数: 1
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 Q4 GEOSCIENCES, MULTIDISCIPLINARY 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 Q4 GEOSCIENCES, MULTIDISCIPLINARY 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 Q4 GEOSCIENCES, MULTIDISCIPLINARY 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 Q4 GEOSCIENCES, MULTIDISCIPLINARY 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 Q4 GEOSCIENCES, MULTIDISCIPLINARY 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 Q4 GEOSCIENCES, MULTIDISCIPLINARY Pub Date : 2021-09-03 DOI: 10.19111/bulletinofmre.990666
H. Alkan, E. Bayrak
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引用次数: 3
期刊
Bulletin of the Mineral Research and Exploration
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