Готові списки джерел за темами / Makran (Iran)

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Добірка наукової літератури з теми "Makran (Iran)"

Автор: Grafiati
Опубліковано: 13 квітня 2024
Оновлено: 25 травня 2024

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Статті в журналах з теми "Makran (Iran)"

1

Hafeez Abbasi, Muhammad Imran. "IS MAKRAN A SEPARATE MICROPLATE? A SHORT REVIEW." MALAYSIAN JOURNAL OF GEOSCIENCES 5, no. 1 (2020): 01–05. http://dx.doi.org/10.26480/mjg.01.2021.01.05.

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Анотація:
Makran Subduction Zone (MZS) is important as this region lies on both sides of the border of Iran and Pakistan along the coastline. Makran Subduction complex has pervasive seismicity and diverse focal mechanism solutions and being in the vicinity of Triple Junction where three major Tectonic plates; Arabian, Eurasian and Indian plates are connecting. Both of Chabahar and Gwadar ports are located in this vicinity, on which China is investing for CPEC, Belt and Road Initiative. The whole world is looking at these projects of Makran, as this may define and transform the future of trade. Hence Geo
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2

Delavar, M. R., H. Mohammadi, M. A. Sharifi, and M. D. Pirooz. "TSUNAMI RISK ASSESSMENT MODELLING IN CHABAHAR PORT, IRAN." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-2/W7 (September 12, 2017): 461–67. http://dx.doi.org/10.5194/isprs-archives-xlii-2-w7-461-2017.

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Анотація:
The well-known historical tsunami in the Makran Subduction Zone (MSZ) region was generated by the earthquake of November 28, 1945 in Makran Coast in the North of Oman Sea. This destructive tsunami killed over 4,000 people in Southern Pakistan and India, caused great loss of life and devastation along the coasts of Western India, Iran and Oman. According to the report of "Remembering the 1945 Makran Tsunami", compiled by the Intergovernmental Oceanographic Commission (UNESCO/IOC), the maximum inundation of Chabahar port was 367 m toward the dry land, which had a height of 3.6 meters from the se
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3

Khan, Waseem, and Mahnoor Mirwani. "PROBING THE NATURE AND CHARACTERISTICS OF ACTIVE MUD VOLCANIC CLUSTERS IN MAKRAN COASTAL ZONE, PAKISTAN." International Journal of Research -GRANTHAALAYAH 8, no. 3 (2020): 214–22. http://dx.doi.org/10.29121/granthaalayah.v8.i3.2020.145.

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Анотація:
Makran Subduction Zone is formed in Late Cretaceous. It is divided into Eastern Makran at the southern edge of Helmand Block in Pakistan and the Western Makran at the southern edge of Lut Block in Iran. The velocity of convergence in Eastern and Western Makran are 42.0 mm/yr and 35.6 mm/yr repectively. Both segments are bound by strike-slip faults e.g. Ornach-Nal left lateral fault in the east and Minab right lateral in the west. Stratigraphically, the zone comprises Formations of ages ranging from Cretaceous to Holocene. In the Eastern Makran, most of the mud volcanoes are located along strik
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4

Normand, Raphaël, Guy Simpson, Frédéric Herman, Rabiul Haque Biswas, and Abbas Bahroudi. "Holocene Sedimentary Record and Coastal Evolution in the Makran Subduction Zone (Iran)." Quaternary 2, no. 2 (2019): 21. http://dx.doi.org/10.3390/quat2020021.

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Анотація:
The western Makran coast displays evidence of surface uplift since at least the Late Pleistocene, but it remains uncertain whether this displacement is accommodated by creep on the subduction interface, or in a series of large earthquakes. Here, we address this problem by looking at the short-term (Holocene) history of continental vertical displacements recorded in the geomorphology and sedimentary succession of the Makran beaches. In the region of Chabahar (Southern Iran), we study two bay-beaches through the description, measurement and dating of 13 sedimentary sections with a combination of
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5

Safari, A., A. M. Abolghasem, N. Abedini, and Z. Mousavi. "ASSESSMENT OF OPTIMUM VALUE FOR DIP ANGLE AND LOCKING RATE PARAMETERS IN MAKRAN SUBDUCTION ZONE." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLII-4/W4 (September 27, 2017): 523–29. http://dx.doi.org/10.5194/isprs-archives-xlii-4-w4-523-2017.

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Анотація:
Makran subduction zone is one of the convergent areas that have been studied by spatial geodesy. Makran zone is located in the South Eastern of Iran and South of Pakistan forming the part of Eurasian-Arabian plate's border where oceanic crust in the Arabian plate (or in Oman Sea) subducts under the Eurasian plate ( Farhoudi and Karig, 1977). Due to lack of historical and modern tools in the area, a sampling of sparse measurements of the permanent GPS stations and temporary stations (campaign) has been conducted in the past decade. Makran subduction zone from different perspectives has unusual
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6

Ayub, Mubarak, and Safi Ullah Khan Marwat. "State and Society under the Zikris in Makran: A Historical Account." Global Social Sciences Review VIII, no. II (2023): 108–18. http://dx.doi.org/10.31703/gssr.2023(viii-ii).11.

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Анотація:
Makran is the South-Western division of Balochistan, Pakistan and the South-Eastern region of Sistan-wa-Balochistan, Iran. Makran has been of great importance to many superpowers of the last thirteen centuries. Macedonians, Sassanid Persians, Sindhi Brahmins, and Arabs had all laid nominal claim to Makran at various times. It has been the battlefield for several ancient powers such as Sassanid, Indians and Greek. Throughout the medieval era, it was dominated by the Arabs and other Central Asian dynasties such as the Seljuks, Ghaznavids and Ghorids. During the 16th century, it was also invaded
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7

Haberland, Christian, Mohammad Mokhtari, Hassan Ali Babaei, et al. "Anatomy of a crustal-scale accretionary complex: Insights from deep seismic sounding of the onshore western Makran subduction zone, Iran." Geology 49, no. 1 (2020): 3–7. http://dx.doi.org/10.1130/g47700.1.

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Abstract The Makran subduction zone has produced M 8+ earthquakes and subsequent tsunamis in historic times, hence indicating high risk for the coastal regions of southern Iran, Pakistan, and neighboring countries. Besides this, the Makran subduction zone is an end-member subduction zone featuring extreme properties, with one of the largest sediment inputs and the widest accretionary wedge on Earth. While surface geology and shallow structure of the offshore wedge have been relatively well studied, primary information on the deeper structure of the onshore part is largely absent. We present th
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8

Normand, Raphaël, Guy Simpson, and Abbas Bahroudi. "Extension at the coast of the Makran subduction zone (Iran)." Terra Nova 31, no. 6 (2019): 503–10. http://dx.doi.org/10.1111/ter.12419.

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9

Negaresh, Hossein. "Mud volcanoes in Sistan and Baluchestan Provinces, Makran Coast, Southeast Iran." Bulletin of the Geological Society of Malaysia 54 (November 1, 2008): 1–7. http://dx.doi.org/10.7186/bgsm54200801.

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10

Nemati, Majid. "Seismotectonic and seismicity of Makran, a bimodal subduction zone, SE Iran." Journal of Asian Earth Sciences 169 (January 2019): 139–61. http://dx.doi.org/10.1016/j.jseaes.2018.08.009.

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Дисертації з теми "Makran (Iran)"

1

Pokharel, Shankar Babu. "Remote Sensing and GIS Analysis of Spatial Distribution of Fracture Patterns in the Makran Accretionary Prism, Southeast Iran." Digital Archive @ GSU, 2007. http://digitalarchive.gsu.edu/geosciences_theses/8.

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Анотація:
This study shows that remote sensing and GIS are powerful tools in identifying geologically induced lineaments from digitally enhanced ETM+ satellite imageries and the digital elevation model (DEM) in remote areas such as the Makran accretionary prism, southeast Iran. The presence of the conjugate shear fractures in the eastern part, along with the extensional, and the presence of reidal sets associated with the subsidiary fractures of the Minab-Zendal fault system in the western part, suggests that the structural pattern changes from pure shear to simple shear from east to the west across the
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2

Regard, Vincent. "Variations temporelle et spatiale de la transition subduction-collision : tectonique de la transition Zagros-Makran (Iran) et modélisation analogique." Phd thesis, Aix-Marseille 3, 2003. http://tel.archives-ouvertes.fr/tel-00003777.

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Анотація:
Les transitions spatiale et temporelle de la subduction à la collision sont des charnières géodynamiques. Nous précisons dans ce travail le rôle et le devenir de ces zones grâce à des modèles analogiques et l'étude tectonique d'un cas réel. La modélisation a montré qu'une transition temporelle entre subduction et collision est toujours marquée par une phase de subduction continentale. La durée de cette phase dépend de la façon dont se déforme la lithosphère subductée en profondeur. Plus elle se déforme, plus courte est la subduction continentale. Dans le cas d'une transition latérale entre sub
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3

Ninkabou, Dia. "Tectono-sedimentary and geodynamic evolution of the Makran Subduction Zone and the Gulf of Oman, from the Late Cretaceous to Present." Electronic Thesis or Diss., Sorbonne université, 2021. http://www.theses.fr/2021SORUS581.

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Анотація:
La zone de subduction du Makran, situé entre les plaques Arabe, Indienne et Eurasienne est caractérisé par l’un des plus grands prisme d’accrétion au monde. D’âge cénozoïque, ce prisme présente de fortes différences dans sa morphologie d’Est en Ouest, à terre et en mer. Afin de déterminer les causes de ces disparités, des données de sismiques réflexion ont été étudiés en mer à travers le prisme et le Golfe d’Oman, nous renseignant sur l’évolution de la zone d’étude à l’échelle du bassin. Des données de tomographie sismique ont aussi été étudiés à travers la région, nous renseignant sur la stru
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4

Shah-Hosseini, Majid. "Geomorphic evolution and coastal hazards along the Iranian coast of Makran." Thesis, Aix-Marseille, 2014. http://www.theses.fr/2014AIXM3010.

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Анотація:
Cette thèse a deux objectifs principaux: (i) la reconstruction de l'évolution des plaines côtières autour des baies de Chabahar et de Pozm et (ii) L'évaluation des risques côtiers (tsunamis et tempêtes extrêmes) par l'étude des dépôts de haute énergie. Vastes plaines côtières et paleo-rivages protégées par des terrasses marines soulevées sont présents autour des baies de Chabahar et Pozm. Nous avons mise en évidence des changements du niveau marin relatif le long de quatre profils. L'architecture interne des paleo-rivages a été imagée en utilisant le géoradar (GPR). Des analyses sédimentologiq
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5

Mutin, Benjamin. "Contribution à l'étude du peuplement des confins indo-iraniens au chalcolithique : caractérisation de la production céramique des périodes II et IIa du Makran pakistanais (4e millénaire avant J.-C.)." Paris 1, 2007. http://www.theses.fr/2007PA010670.

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Анотація:
Le programme de recherche archéologique mis en place par R. Besenval, il y a vingt ans au Makran pakistanais (Sud-Ouest du Pakistan), a comblé un manque de données important relatif au peuplement ancien de cette région localisée à mi-chemin des cultures du Plateau iranien et du Pakistan oriental. La fouille des sites de la vallée de la Kech et les prospections conduites dans la région ont permis de restituer la chronologie de son occupation humaine dont les premières traces datent du 5e millénaire avant J. -C. Tout en révélant une riche nature matérielle et une forte occupation aux époques sui
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6

BARBERO, EDOARDO. "Geological and petrological investigation of the western North Makran ophiolites (SE Iran): new constraints for the Late Jurassic – Cretaceous tectono-magmatic and geodynamic evolution of the Neo-Tethys Ocean." Doctoral thesis, Università degli studi di Ferrara, 2021. http://hdl.handle.net/11392/2488101.

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Анотація:
The Makran Accretionary Prism (South Iran) is related to the convergence between the Arabia and Eurasia plates accommodated by the northward subduction of the Neo-Tethys Ocean since the Cretaceous. Mesozoic ophiolites, sedimentary successions, and minor continental-derived tectonic units are preserved in the North Makran domain. This thesis is focused on field-based geological study, as well as petrological and geochemical characterization of the magmatic rocks of the Bajgan and Durkan Complexes, the Band-e-Zeyarat ophiolitic unit, and the Ganj Complex The studied units are included in the No
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7

Yamini, Fard Farzam. "Sismotectonique et structure lithosphérique de deux zones de transition dans le Zagros (Iran) : la zone de Minab et la zone de Qatar-Kazerun." Phd thesis, Grenoble 1, 2003. http://tel.archives-ouvertes.fr/tel-00707751.

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Анотація:
Les failles importantes en coulissage orientées NS comme la faille du Zendan-Minab-Palami (ZMP) et la faille de Borazjan-Kazerun-Dena séparent des styles différents de déformation au sud de l'Iran. Le ZMP sépare la zone de collision du Zagros à la zone de subduction du Makran. Nous utilisons des données microsismiques et téléséismiques enregistrées par un réseau temporaire de 50 stations qui a fonctionné en novembre et décembre 1999. La microsismicité observée dans cette région montre une activité diffuse entre la faille de Zendan-Minab-Palami et la faille de Jiroft, limitée par la dépression
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8

Karlsson, Simon. "Makten på Öland och i Möre : Järnålderns elit i ett lokalt perspektiv." Thesis, University of Kalmar, School of Human Sciences, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:hik:diva-213.

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<p>The social elite on Öland and in Möre in the south east of Sweden during the Iron Age is described on the basis of the archaelogical record, such as graves, settlements and traces of pre-Christian central places. The material is discussed to see if traces of an elite are to be found. The power configuration between Öland and Möre is also discussed.</p><p> </p>
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9

Winbergh, Göran. "Elit och tvång, eller släkt och rådslag? : Två tolkningar av makten på Gotland under romersk järnålder." Thesis, Uppsala universitet, Institutionen för arkeologi och antik historia, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-391121.

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Анотація:
In the archaeological research about the Baltic Sea island of Gotland during Roman Iron Age, 0–400 AD, two different approaches are visible: One that sees the community life on Gotland as different from the one on the main land with a relative stabile development, based on the family and kin, where no higher elite separate itself. The other perception emanates from the changes in southern Scandinavia, where an elite steadily grows and finally isolate itself as an aristocracy with unlimited power over others, the development on Gotland is no exception. This paper is about describing, investigat
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10

Moore, Martyn Patrick John. "The Iron Age of the Makapan Valley area, central Transvaal." Thesis, 2015. http://hdl.handle.net/10539/17046.

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Thesis (M.A.)--University of the Witwatersrand, Faculty of Arts, 1981.<br>A culture-history research project was initiated for the relatively unresearched Makapan Valley area of the central Transvaal. The valley was surveyed intensively and fifty sites recorded. Three, 2429AA4 (Ficus), 2429AA24 (Kekane) and 2429AA36 were excavated. Ficus was a multicomponent site with four phases of occupation; an initial fifth to sixth century A.D. Lydenburg phase, a ninth to tenth century Eiland phase, an ambiguous fifteenth century entity and a superficial early twentieth century Ndebele occupation.
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Книги з теми "Makran (Iran)"

1

Mardiyati, Umi. Peranan angkutan laut dalam penyediaan bahan makanan di Irian Jaya: Laporan penelitian. Jurusan Ekonomi, Fakultas Ilmu Sosial dan Ilmu Politik, Universitas Cenderawasih, 1993.

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2

Kjeldsen, Jens E., and Siri Meyer, eds. Krig, rett & retorikk – en bok om kommunikasjonsregimer. 3rd ed. Retorikförlaget, 2004. http://dx.doi.org/10.52610/fhhn6728.

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Krigen, retten og retorikken. Hvordan påvirker de hverandre og hvordan er de med på å skape samfunn og sosiale realiteter? Boken handler om ”kommunikasjonsregimer”: et sett av retoriske former og tankefigurer som setter seg gjennom som dominerende måter å tenke og tale på innenfor bestemte samfunnsfelt. Et kommunikasjonsregime betinger hva som kan bli sagt, representert, få en kommunikativ form. Krig, rett og retorikk viser hvordan forskjellige kommunikasjonsregimer gjorde det mulig retorisk å fusjonere hendelsene 11. september 2001 med legitimeringen av invasjonen av Irak. Det skapte en situa
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3

Wahyudhi, Nostalgiawan, ed. Many Faces of Political Islam in the Middle East: Arah Baru Gerakan Politik Islam Pasca-Arab Spring. LIPI PRESS, 2020. http://dx.doi.org/10.14203/press.294.

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Arab spring membawa perubahan besar pada politik Timur Tengah. Banyak yang berharap bahwa Arab spring bukan hanya revolusi Arab jilid dua setelah revolusi Iran pada tahun 1979, tetapi merupakan era baru kebangkitan demokratisasi di Timur Tengah yang akan memberi ruang bagi gerakan politik Islam berpartisipasi secara terbuka di ranah publik. Sarjana-sarjana studi Islam beranggapan bahwa Arab spring merupakan jembatan menuju “Islamist winter”. Islamist winter diartikan dengan ketakutan dunia akan tumbuhnya kalangan Islamis menguasai kekuasaan di dunia Arab.[1] Hal ini mengarah pada notasi apakah
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Частини книг з теми "Makran (Iran)"

1

Burg, J. P., A. Dolati, D. Bernoulli, and J. Smit. "structural style of the Makran Tertiary accretionary complex in SE-Iran." In Lithosphere Dynamics and Sedimentary Basins: The Arabian Plate and Analogues. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-30609-9_12.

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Dolati, A., and J. P. Burg. "Preliminary fault analysis and paleostress evolution in the Makran Fold-and-Thrust Belt in Iran." In Lithosphere Dynamics and Sedimentary Basins: The Arabian Plate and Analogues. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-30609-9_13.

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Barbero, Edoardo, Morteza Delavari, Asghar Dolati, et al. "New Geochemical and Age Data on the Bajgan Complex (Makran Accretionary Prism, SE Iran): Implications for the Redefinition of Its Tectonic Setting of Formation from a Paleozoic Continental Basement to a Cretaceous Oceanic Domain." In Recent Research on Sedimentology, Stratigraphy, Paleontology, Tectonics, Geochemistry, Volcanology and Petroleum Geology. Springer Nature Switzerland, 2023. http://dx.doi.org/10.1007/978-3-031-43222-4_35.

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4

Susilawati, Euis. "Pentingnya APSCO bagi Pembangunan Keantariksaan Indonesia." In Kajian Kebijakan dan Informasi Kedirgantaraan. Mitra Wacana Media, 2015. http://dx.doi.org/10.30536/9786023181360.7.

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APSCO merupakan organisasi kerja sama multilateral keantariksaan yang dibentuk oleh delapan negara di Asia Pasifik pada tahun 2005 di Beijing, Tiongkok. Indonesia merupakan salah satu negara penandatangan Konvensi APSCO, namun sampai sekarang belum menjadi anggota karena belum meratifikasi Konvensi tersebut. Apabila Indonesia menjadi anggota APSCO maka setiap tahunnya Indonesia harus membayar kontribusi pendanaan dan tentunya akan menambah beban anggaran pemerintah Indonesia. Untuk itu harus dibuktikan bahwa dengan kontribusi yang dibayarkan tersebut dapat memberikan manfaat bagi pembangunan keantariksaan untuk jangka pendek, jangka menengah, dan jangka panjang. Kajian ini bertujuan menganalis pentingnya APSCO bagi pembangunan keantariksaan yang dilihat tidak hanya menilai manfaat yang diperoleh dari sisi kontribusi pendanaan yang diberikan. Metoda yang digunakan dalam kajian ini adalah deskriptif, dan dengan menggunakan perspektif politik, analisis menghasilkan bahwa secara politik dalam APSCO sangat penting bagi Indonesia yang dapat dimanfaatkan sebagai wahana untuk promosi kemampuan Indonesia dalam aplikasi keantariksan kepada negara-negara anggota APSCO, dan memperoleh alih teknologi antariksa (peroketan) dari Tiongkok atau Iran melalui kegiatan atau program pengembangan teknologi antariksa, atau kegiatan pilihan lainnya yang disepakati bersama yang tidak terdapat dalam organisasi multilateral lainnya sejenis seperti APRSAF dan UNCSSTEAP.
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"UPLIFTED MARINE TERRACES ALONG THE MAKRAN COAST OF PAKISTAN AND IRAN." In Himalaya to the Sea. Routledge, 2002. http://dx.doi.org/10.4324/9780203414637-27.

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Aubourg, C., B. Smith, H. Bakhtari, et al. "Post-Miocene shortening pictured by magnetic fabric across the Zagros-Makran syntaxis (Iran)." In Special Paper 383: Orogenic curvature: Integrating paleomagnetic and structural analyses. Geological Society of America, 2004. http://dx.doi.org/10.1130/0-8137-2383-3(2004)383[17:pspbmf]2.0.co;2.

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Postma, Dirk Willem. "Kwetsbaar burgerschap: Naar een vrijplaats voor boeren, burgers en buitenlui." In Geleefd Burgerschap: Van eenheidsdwang naar ruimte voor verschil en vitaliteit. Uitgeverij SWP, 2012. http://dx.doi.org/10.36254/978-90-8850-334-4.10.

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Het is woensdag 16 februari 2011, tien uur ‘s ochtends op buurtboerderij Ons Genoegen aan de groene rafelrand van het Amsterdamse Westerpark. Een waterig winterzonnetje doet zijn uiterste best om door de wolken heen te breken. Op het terras wordt een sigaretje gerookt door de schoonmaker en twee medevrijwilligers die vandaag de bar en keuken bestieren. Zij vragen een gast die nogal luidruchtig met zijn zoon speelt om rekening te houden met de workshop Mindfulness die op dat moment op de zolderverdieping van de boerderij plaatsvindt. Aan de rand van het erf legt de tuingroep een composthoop aan en vlechten een hek van wilgentakken die de week daarvoor zijn gesnoeid op de naastgelegen begraafplaats Sint Barbara. Sommige takken zijn al kaalgevreten door de schapen en geiten. Bij vorst krijgen zij deze takken als ruwvoer. Door het weiland tussen de begraafplaats en de boerderij komt Rob aangelopen. De schapen en geiten volgen hem op de voet naar de stal, waar de dieren worden gevoerd. Bij de stal aangekomen, groet hij de twee mannen die zich daar omkleden voor het leegpompen van de greppels in het deels onder water gelopen weiland. Er wordt nog even nagepraat over de geit die de dag daarvoor door de schoonmaker uit een benarde positie was bevrijd; deze hing met een pootje aan de hoge ruif op de kar en kon met zijn andere pootje niet bij de grond. Sindsdien loopt het geitje mank, ze houdt haar rechtervoorpootje omhoog. Dit incident wordt het gesprek van de dag; alle vrijwilligers en bezoekers van de boerderij maken zich zorgen. Ze stellen vragen aan de schoonmaker, die in de noordelijke bergen van Irak tussen de geiten is opgegroeid, en geven – gevraagd en ongevraagd – adviezen aan de weilandwerkers.
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Тези доповідей конференцій з теми "Makran (Iran)"

1

Heidarzadeh, Mohammad, Moharram D. Pirooz, Nasser H. Zaker, and Mohammad Mokhtari. "Modeling of Tsunami Propagation in the Vicinity of the Southern Coasts of Iran." In ASME 2007 26th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2007. http://dx.doi.org/10.1115/omae2007-29082.

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The extensive death toll and sever economical damages brought by the 2004 Indian Ocean tsunami has emphasized the urgent need for assessing the hazard of tsunami in this ocean, and determining the most vulnerable coastlines to the impact of possible tsunami. In this paper the hazard of tsunami for southern coasts of Iran bordering the Indian Ocean is discussed. At first, historical data of tsunami occurrences on the Iranian southern coasts are collected, described and analyzed. Then, numerical simulation of potential tsunamis in the Makran subduction zone is performed and the tsunami wave heig
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2

Grando, Gianluca, and Ken McClay. "Subduction-related deformation processes in the Makran accretionary prism, offshore Iran." In GEO 2008. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.246.158.

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3

"Probabilistic Tsunami Hazard of Splay and Normal Faults in the Western Makran/Iran." In The Second Eurasian RISK-2020 Conference and Symposium. AIJR Publisher, 2020. http://dx.doi.org/10.21467/abstracts.93.2.

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4

Khiabani Moghadam, Arash. "GEOCHEMISTRY AND PETROLOGY OF GABBRO INTRUSIONS AND ULTRAMAFIC ROCKS FROM WESTERN MARGIN OF MAKRAN ACCRETIONARY WEDGE (COLOURED MELANGE) COMPLEX, SE IRAN." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-348921.

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5

Dafrina, Armelia, Deassy Siska, and Maulana Hakiki. "Identifikasi Pengaruh Arsitektur Timur Tengah pada Desain Masjid Raya Pase Panton Labu." In Temu Ilmiah IPLBI 2021. Ikatan Peneliti Lingkungan Binaan Indonesia, 2021. http://dx.doi.org/10.32315/ti.9.i023.

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Perkembangan zaman memberikan pengaruh pada seni arsitektur, salah satunya perkembangan seni arsitektur pada masjid. berdasarkan dari bentuk sebuah masjid mengacu pada sejarah kejayaan dinasti Islam pada masa lampau yang meninggalkan bangunan masjid dengan karakteristik atau ciri-ciri bentuk masjid berdasarkan peninggalan beberapa masa yang berbeda yakni Abbasiyah (Mesir/Mesopotamia), Ummayah (Andalusia/Spanyol), Safavid (Iran), Mughal (India), Utsmaniyah (Turki).Timur Tengah merupakan istilah oleh bangsa Inggris untuk wilayah yang mayoritas umat Islam. Wilayah tersebut disebutkan berdasarkan
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