پیوندهای مفید
اخبار و اعلانات
آمار
| تعداد نشریات | 158 |
| تعداد شماره‌ها | 6,225 |
| تعداد مقالات | 67,685 |
| تعداد مشاهده مقاله | 114,991,947 |
| تعداد دریافت فایل اصل مقاله | 89,660,926 |
مطالعه ساختار لیتوسفر شمالغرب ایران با استفاده از تابع گیرنده S | ||
| فیزیک زمین و فضا | ||
| مقاله 5، دوره 46، شماره 2، مرداد 1399، صفحه 265-276 اصل مقاله (930.22 K) | ||
| نوع مقاله: مقاله پژوهشی | ||
| شناسه دیجیتال (DOI): 10.22059/jesphys.2020.295106.1007185 | ||
| نویسندگان | ||
| وحیده قربانعلی‌زاده1؛ سیدخلیل متقی* 2؛ فرهاد ثبوتی* 3 | ||
| 1دانش‌آموخته کارشناسی ارشد، دانشکده علوم زمین، دانشگاه تحصیلات تکمیلی علوم پایه، زنجان، ایران | ||
| 2استادیار، دانشکده علوم زمین، دانشگاه تحصیلات تکمیلی علوم پایه، زنجان، ایران | ||
| 3دانشیار، دانشکده علوم زمین، دانشگاه تحصیلات تکمیلی علوم پایه، زنجان، ایران | ||
| چکیده | ||
| در این مقاله نتایج تحلیل و مهاجرت به عمق توابع گیرنده S در شمالغرب ایران ارائه میشود. شبکه لرزهنگاری مورد استفاده در این مطالعه شامل 23 ایستگاه باند پهن و متوسط است که از ساحل غربی دریای خزر آغاز شده و تا ساحل شرقی دریاچه ارومیه در امتداد یک خط تقریباً مستقیم با جهتگیری شرقی-غربی و عمود بر رشتهکوههای تالش ادامه مییابد و از مجاورت آتش‌فشانهای سهند و سبلان میگذرد. زلزلههای دورلرز ثبت شده از زلزلههای رخداده در فاصله رومرکزی 55 درجه تا 85 درجه و بزرگای بیش از 5/5 که از بانک داده جمعآوری شده در بازه زمانی آگوست 2008 تا جولای 2012 استخراج شدند و توابع گیرنده S با واهمامیخت مؤلفه شعاعی از مؤلفه قائم به‌دست آمد. نتایج حاصل از برهمانبارش این توابع گیرنده S نشان میدهد که شمالغرب ایران دارای لیتوسفر نسبتا نازکی است که ضخامت آن در بیشتر مناطق برابر با 10±80 کیلومتر است و در زیر سبلان به 10±120 کیلومتر افزایش مییابد. به‌نظر میرسد نازک بودن لیتوسفر تطابق نزدیکی با وجود بیهنجاریهای دمایی در شمالغرب ایران دارد. پوسته و لیتوسفر در زیر آتش‌فشان سبلان نسبت به نواحی اطراف ضخیمتر است که میتواند ناشی از همگرایی بلوک خزر جنوبی و لیتوسفر قارهای شمالغرب ایران باشد. به‌علاوه نتایج ما یک پله در مرز موهو در زیر کوه‌های تالش را آشکار میکند که به‌نظر میرسد به‌علت مجاورت پوسته خزر جنوبی و پوسته قارهای شمالغرب ایران در این منطقه باشد. | ||
| کلیدواژه‌ها | ||
| شمالغرب ایران؛ تابع گیرنده S؛ مرز موهو؛ ضخامت لیتوسفر | ||
| عنوان مقاله [English] | ||
| Lithospheric Structure of the NW Iran revealed by S Receiver Functions | ||
| نویسندگان [English] | ||
| Vahideh Ghorbanalizadeh1؛ Seyed Khalil Motaghi2؛ Farhad Sobouti3 | ||
| 1M.Sc. Graduated, Department of Earth Sciences, Institute for Advanced Studies in Basic Sciences, Zanjan, Iran | ||
| 2Assistant Professor, Department of Earth Sciences, Institute for Advanced Studies in Basic Sciences, Zanjan, Iran | ||
| 3Associate Professor, Department of Earth Sciences, Institute for Advanced Studies in Basic Sciences, Zanjan, Iran | ||
| چکیده [English] | ||
| Iran Plateau is part of the Alpine-Himalayan orogenic system in western Asia. It is located in a seismically active region affected by a transpressional tectonic regime of oblique convergence, generated by the convergence of the Arabian plate toward Eurasia. The current morphology of Iranian plateau had been dominated by opening and closing of the Paleo-Tethys and Neo-Tethys oceans in the past. Current lithospheric deformation in the NW Iran is shaped by the convergence of Arabia and Eurasia and the westward motion of the rigid South Caspian Basin. The South Caspian Basin is a relatively aseismic rigid basement block and has affected the deformation history of its surrounding continental regions. The South Caspian Basin and the Kura depression to its west are thought to be a relic back-arc of the Tethyan Mesozoic subduction caught up in a continental collision zone similar to the Black Sea and the eastern Mediterranean. The South Caspian Basin is a piece of unusually-thick oceanic-like crust, because of its low elevation and its west and southward motion relative to central Iran. Here we present results of a S-receiver function analysis for a 290 km long temporary seismic network in the NW Iran. The network is a linear array stretching from the western coast of the South Caspian Basin to the Lake Urumieh. We computed the individual S receiver functions for 23 broad-band seismic stations and then we stacked them based on their piercing points at depth of 80 km. To calculate S receiver functions, the teleseismic S waveforms were cut from 200 s before to 100 s after the theoretical S wave onset. ZNE-component waveforms were rotated into the ZRT coordinate system and the R component was deconvolved from the Z component. To make S receiver functions similar to P receiver functions, we reversed the time axis and the polarity of S receiver function time series. The Gaussian smoothing factor was selected equal to 1.0 for both data sets, which is equivalent to the application of a Gaussian low pass filter with a corner frequency of ~0.2 Hz to the receiver functions. Piercing points at north and south of the linear profile were separated into two different data sets to avoid the stacking of 3D heterogeneities. Stacking receiver functions confirms a thin crust east of the Talesh Mountains juxtaposing with a thick continental crust beneath the NW Iran. We interpret the thin crust as an oceanic-like crust belonging to the South Caspian Basin. The detected Lithosphere-Asthenosphere boundary is almost shallow with an average depth of ~100 km. However, its variations across the profiles are different in each data set. Variations beneath the region south of the profile are minor revealing a flat, thin lithosphere beneath the region. The lithosphere (as well as crust), however, becomes thick beneath Sabalan volcano, north of the profile, probably due to convergence of the NW Iran and the South Caspian basin above the North Tabriz Fault. This interpretation implies that the North Tabriz Fault is a continental suture between the NW Iran and Central Iran plateau. | ||
| کلیدواژه‌ها [English] | ||
| NW Iran, S receiver function, Moho boundary, Lithospheric thickness | ||
| مراجع | ||
|
Al-Lazki, A. I., Sandvo, E., Seber, D., Barazangi, M., Turkelli, N. and Mohaman, R., 2004, Pn tomographic imaging of mantle lid velocity and anisotropy at the junction of the Arabian, Eurasian, and African plates, Geophys. J. Int.,158, 1024-1040. Amini, S., Shomali, Z. H., Koyi, H. and Roberts, R. G., 2012, Tomographic upper-mantle velocity structure beneath the Iranian Plateau. Tectonophysics, 554, 42-49. Angus, D. A., Wilson, D. C., Sandvol, E. and Ni, J. F., 2006, Lithospheric structure of the Arabian and Eurasian collision zone in eastern Turkey from S-wave receiver functions. Geophysical Journal International, 166(3), 1335-1346. Azizzanjani, A., Ghods, A., Sobouti, F., Bergman, E., Mortezanejad, G., Priestley, K., Madanipour, S. and Rezaeian, M., 2013, Seismicity in the western coast of the South Caspian Basin and the Talesh Mountains, Geophysic. J. Int., 195, 799-814. Bavali, K., Motaghi, K., Sobouti, F., Ghods, A., Abbasi, M., Priestley, K., Mortezanejad, G. and Rezaeian, M., 2016, Lithospheric structure beneath NW Iran using regional and teleseismic travel-time tomography, Physic of the Earth and Planetary Interiors.253, 97-107. Chen, L., Zheng, T. and Xu, W., 2006, A thinned lithospheric image of the Tanlu Fault Zone, eastern China: Constructed from wave equation based receiver function migration, Journal of Geophysical Research, B09312 (111), doi:10.1029/2005JB003974. Chiu, H. Y., Chung, S. L., Zarrinkoub, M. H., Mohammadi, S. S., Khatib, M. M. and Iizuka, Y., 2013, Zircon U–Pb age constraints from Iran on the magmatic evolution related to Neotethyan subduction and Zagros orogeny, Lithos, 162–163, 70–87. Ghods, A., Shabanian, E., Bergman, E., Faridi, M., Donner, S., Mortezanejad, Gh. and Aziz-Zanjani, A., 2015, The Varzaghan-Ahar, Iran, Earthquake Doublet (Mw 6.4, 6.2): implications for the geodynamics of northwest Iran. 203,522-540. Gök, R., Pasyanos, M. E. and Zor, E., 2007, Lithospheric structure of the continent—continent collision zone: eastern Turkey. Geophysical Journal International, 169(3), 1079-1088. Hearn, T. M. and Ni, J. F., 1994, Pn velocities beneath continental collision zones: the Turkish-Iranian Plateau. Geophysical Journal International, 117(2), 273-283. Hessami, K., Pantosti, D., Tabasi, H., Shabanian, E., Abbasi, M. R., Feghhi, K. and Soleymani, S., 2003, Paleoearthquakes and slip rates of the North Tabriz Fault, NW Iran: preliminary results, Annals of Geophysics, 46 (5), 903-915. Jackson, J., 1992, Partitioning of strike-slip and convergent mountain between Eurasia and Arabia in Eastern Turkey and the Caucasus, J. Geophys. Res, 97,471-479. Kennett, B. L. N. and Engdahl, E. R. 1991, Traveltimes for global earthquake location and phase identification. Geophysical Journal International, 105(2), 429-465. Khorrami, F., Vernant, P., Masson, F., Nilfouroushan, F., Mousavi, Z., Nankali, H., Saadat, S.A., Walpersdorf, A., Hosseini, S., Tavakoli, P. and Aghamohammadi, A. 2019, An up-to-date crustal deformation map of Iran using integrated campaign-mode and permanent GPS velocities. Geophysical Journal International, 217(2), 832-843. Lü, Y., Ni, S., Chen, L. and Chen, Q. F. 2017, Pn tomography with Moho depth correction from eastern Europe to western China. Journal of Geophysical Research: Solid Earth, 122(2), 1284-1301. Maggi, A. and Priestley, K., 2005, Surface Waveform Tomography of the Turkish-Iranian Plateau, Geophys. J. Int., 160, 1068-1080. McKenzie, D. and Priestley, K. 2008, The influence of lithospheric thickness variations on continental evolution. Lithos, 102(1-2), 1-11. Priestley, k., McKenzie, D., Barron, J., Tatar, M., and Debayle, E., 2012, The Zagros core: Deformation of the continental lithospheric mantle Geochemistry Geophysics Geosystems, v. 13, Q11014, doi:10.1029/2012GC004435. Schulte-Pelkum, V. and Mahan, K. H., 2014, A method for mapping crustal deformation and anisotropy with receiver functions and first results from USArray. Earth and Planetary Science Letters, 402, 221-233. Taghizadeh-Farahmand, F., Sodoudi, F., Afsari, N. and Ghassemi, M. R., 2010, Lithospheric structure of NW Iran from P and S receiver functions. Journal of seismology, 14(4), 823-836. Taghizadeh Farahmand, F. and Afsari, N., 2018, Variation of Lithosphere-Asthenosphere boundary beneath Iran by using S Receiver function. Iranian Journal of Earth Sciences, 10(1), 11-19. | ||
|
آمار تعداد مشاهده مقاله: 593 تعداد دریافت فایل اصل مقاله: 333 |
||