Bibliografías temáticas / 998-1030

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Literatura académica sobre el tema "998-1030"

Autor: Grafiati
Publicado: 26 de julio de 2024
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "998-1030"

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Rahmawati, Rahmawati, Nor Huda, and Otoman Otoman. "PERAN MAHMUD GHAZNI TERHADAP PERKEMBANGAN PERADABAN ISLAM, 388-421 H/ 998-1030 M." Tanjak: Sejarah dan Peradaban Islam 1, no. 2 (2021): 21–41. http://dx.doi.org/10.19109/tanjak.v1i2.9373.

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The topic of this research needs to be investigated because at that time there were many events related to the description of the struggle of many Islamic figures in advancing Islam, especially Mahmud Ghazni. During the reign of Mahmud Ghazni Islamic civilization experienced rapid progress and during the reign of Mahmud Ghazni much progress in the fields of education and the economy. Mahmud Ghazni was a man who controlled Islam and had a lot of influence and power during wars and often won over his enemies until the caliph Al-Qadir Billah gave him the title Yamin addaulah which means people wh
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2

حتاملة, عبد الکریم عبده. "دور السلطان محمود الغزنوى فى القضاء على المذهب الکرامى : (387 - 322 هــ / 998 - 1030 م)". مجلة الآداب والعلوم الإنسانیة 36, № 2 (2000): 121–44. http://dx.doi.org/10.21608/fjhj.2000.133441.

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Auer, Blain. "Marriage, Political Alliance, and Imperial Polities in Early Ghaznavid History." Afghanistan 6, no. 1 (2023): 1–28. http://dx.doi.org/10.3366/afg.2023.0101.

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This article considers how marriages were utilized in early Ghaznavid history to forge political alliances, establish relationships of power and to bind together different royal family households. Marriage was employed as a diplomatic tool to ease political tensions and to strengthen coalitions. The Ghaznavid ruler Maḥmūd (r. 388–421/998–1030) utilized marriage alliances with great success to consolidate and expand his territories. In 391/1001, he forged a coalition with the Karakhanids through a marriage to the daughter of Naṣr b. ʿAlī (d. 403/1012–3). In 406/1015–16, Maḥmūd married his own s
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4

حمد عطية, د. علي. "السفارات في العصر الغزنوي". مجلة العلوم والدراسات الإنسانية - كلية الآداب والعلوم – المرج, № 1 (5 травня 2024): 111–29. http://dx.doi.org/10.37376/jsh.vi1.4884.

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ينتسب الغزنويين الى عاصمتهم مدينة غزنة الأفغانية التي تقع على سفوح جبال سليمان , والتي وردت فى المصادر الجغرافيةالعربية باسم (غزنين) و(غزنى) والتى بدأت فى الظهور فى نهاية القرن الرابع الهجرى عندما أتخذها الغزنويين عاصمة لهموامتدت وتوسعت في إقليم خراسان ومعظم بلاد الهند .ويعتبر السلطان سبكتكين المؤسس الحقيقي للدولة الغزنوية والذى ورثه ابنه السلطان محمود 388 − 421 ه/ 998 −1030 م , والذى أمتاز عهده بالجهاد الإسلامي فى إقليم الهند , والذى وصلت غزواته الى حدود هضبة الدكن , واليه يرجعالفضل فى نشر وتثبيت الإسلام فى الهند كما أزال سلطان البويهيين فى الري وبلاد الجبل , كما حارب الأتراك الغزية السلجوقية
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Barber, Bernard. "Parsons’s second project: The social system. Sources, development and limitations." American Sociologist 29, no. 2 (1998): 77–82. http://dx.doi.org/10.1007/s12108-998-1030-y.

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Ferreira, Monica. "The 1997 IFA global conference: A look back." Ageing International 24, no. 4 (1998): 123–28. http://dx.doi.org/10.1007/s12126-998-1030-9.

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Wilson, Edward O. "The case for consilience: A summation." Academic Questions 11, no. 3 (1998): 68–71. http://dx.doi.org/10.1007/s12129-998-1030-y.

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ÖNTÜRK, Vural. "Poets of The Ghaznavid Period In The History of Firiştah of Muhammed Kâsım Hındushah Esterabâdî." JOURNAL OF HISTORY AND FUTURE 9, no. 3 (2023): 503–20. http://dx.doi.org/10.21551/jhf.1350470.

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Gazneliler devri (963-1187) edebî bakımdan son derece önemli bir zamana tesadüf etmektedir. Sultanların her türlü koşulda edebî faaliyetleri desteklemesi, bu türün gelişmesini ve başta Şehnâme olmak üzere birçok kıymetli eserin kaleme alınıp günümüze kadar ulaşmasını sağlamıştır. Diğer ilimlerin yanı sıra şairlik de yine Gazneliler zamanında revaçta bir sanatsal faaliyet olarak karşımıza çıkmaktadır. Bilhassa Sultan Mahmûd döneminde hızlı bir gelişme gösteren şairlik ve şiir yazma geleneği bu tür ile uğraşanlar için aynı zamanda bir geçim kapısı olmuştur. Yalnız Sultan Mahmûd'un her daim dört
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العمرى, عمر بن صالح بن سليمان. "فتوحات السلطان محمود الغزنوي في بلاد الهند 998 - 1030 م". مجلة اتحاد الجامعات العربية للآداب, 2016, 199. http://dx.doi.org/10.51405/0639-013-001-009.

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Annucci, Arturo. "The Coinage of Maḥmūd b. Sebüktegin: Overview and Update of the Monetary History". Annali Sezione Orientale, 15 серпня 2024, 1–17. http://dx.doi.org/10.1163/24685631-12340148.

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Abstract The reign of the Ghaznavid emir Maḥmūd b. Sebüktegin (388–421/998–1030) was a turning point in the monetary history of the Iranian territories. The innovations introduced by his father were maintained and further spread thanks, above all, to the numerous military conquests that resulted in an increase in the number of mints. In this study, we offer a summary of his main issues, new readings and contexts of legends on bronze coins and an overview of the official protocol of this ruler.
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Libros sobre el tema "998-1030"

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al-Sulṭān Maḥmūd al-Ghaznawī: Siyāsatuhu, wa-dawruhu fī nashr al-Islām fī shibh al-qārrah al-Hindīyah, 388-421 H/998-1030 M. Dār Jāmiʻat ʻAdan lil-Ṭibāʻah wa-al-Nashr, 2006.

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Capítulos de libros sobre el tema "998-1030"

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Volkert, Richard A. "Geologic Setting of Proterozoic Iron, Zinc, and Graphite Deposits, New Jersey Highlands." In Part I. Proterozoic Iron and Zinc Deposits of the Adirondack Mountains of New York and the New Jersey Highlands Part II. Environmental Geochemistry and Mining History of Massive Sulfide Deposits in the Vermont Copper Belt. Society of Economic Geologists, 2001. http://dx.doi.org/10.5382/gb.35.07.

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Abstract The New Jersey Highlands are underlain principally by Mesoproterozoic rocks that were metamorphosed at upper amphibolite to granulite facies between 1080 and1030 Ma during the Ottowan Orogeny. The oldest rocks are inferred to be metamorphosed ca. 1300 Ma dacite, tonalite, and trondhjemite and associated charnockitic plutonic and metavolcanic rocks of the Losee Metamorphic Suite. These originated in a continental margin magmatic arc setting dominated by calc-alkaline and tholeiitic magmatism. Rocks of the Losee record a compressional event in the north-central Appalachians that was lik
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