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Journal articles on the topic 'Pyu'

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Published: 4 June 2021

Last updated: 25 July 2025

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1

Kyaw, T., and A. Hoosen. "Obituary: Dr Pyu Pyu Sein (1951–2008)." Southern African Journal of Epidemiology and Infection 24, no. 2 (2009): 36. http://dx.doi.org/10.1080/10158782.2009.11441340.

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2

Miyake, Marc. "Studies in Pyu Phonology, ii: Rhymes." Bulletin of Chinese Linguistics 11, no. 1-2 (2018): 34–76. http://dx.doi.org/10.1163/2405478x-01101008.

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The extinct Pyu language was spoken during the first millennium CE and the early centuries of the second millennium CE in what is now Upper Burma. Pyu appears to be Sino-Tibetan on the basis of its basic vocabulary. It survives in inscriptions in an Indic script. This study reconstructs Pyu rhymes on the basis of spellings in those inscriptions and concludes that Pyu was an atonal language with 7 vowels and 18 final consonants. Some previous scholars have interpreted the subscript dots of the Pyu script as tone markers, but this study argues that they indicate fricative initials.

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3

Miyake, Marc, and Julian Wheatley. "Studies in Pyu Epigraphy II. Pyu Inscriptions on Molded Tablets: A Way Forward?" Journal of Burma Studies 28, no. 1 (2024): 73–123. http://dx.doi.org/10.1353/jbs.2024.a923230.

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Abstract: The Pyu language is known from some 150 inscriptions, a few of them long and most of them short. Almost none can be reliably dated, but paleographical and archeological evidence suggests that the earliest dates from the first half of the first millennium CE. Decipherment of the Pyu language has, thus far, been based mostly on bilingual or multilingual inscriptions. Such inscriptions are few, so further progress will have to be based on monolingual ones. This paper examines a set of short Pyu monolingual inscriptions found mostly on molded tablets. Molded tablets (also called votive t

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4

Miyake, Marc. "A first look at Pyu grammar." Linguistics of the Tibeto-Burman Area 42, no. 2 (2019): 150–221. http://dx.doi.org/10.1075/ltba.18013.miy.

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Abstract Pyu, an extinct Sino-Tibetan language once spoken in what is now Upper Burma, remains barely explored beyond the level of transliterating texts and the identification of individual words. Knowledge of Pyu grammar has advanced little over the past century. This article (1) presents a methodology for discovering the syntax of Pyu, (2) identifies five word classes and their combinatorial properties, (3) lists all known grammatical morphemes with notes on usage, (4) formulates rules of word order, and (5) demonstrates how all of the above can elucidate the meaning of a previously undeciph

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5

Miyake, Marc. "Studies in Pyu phonology, I." Language and Linguistics / 語言暨語言學 22, no. 1 (2020): 28–70. http://dx.doi.org/10.1075/lali.00077.miy.

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Abstract The extinct Pyu language was spoken during the first millennium CE and the early centuries of the second millennium CE in what is now Upper Burma. It has been classified as Sino-Tibetan on the basis of basic vocabulary, but its precise position within the family remains unknown. It survives in inscriptions in an Indic script. In this study, the first of its kind, I begin to reconstruct Pyu phonology on the basis of spellings in those inscriptions. I propose that Pyu was a sesquisyllabic language with 7 preinitials and 43 or 44 initials.

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6

Griffiths, Arlo, and Julian Wheatley. "Five Contributions to Pyu Studies: Introduction." Journal of Burma Studies 28, no. 1 (2024): 1–9. http://dx.doi.org/10.1353/jbs.2024.a923227.

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7

Stargardt, Janice. "From the Iron Age to early cities at Sri Ksetra and Beikthano, Myanmar." Journal of Southeast Asian Studies 47, no. 3 (2016): 341–65. http://dx.doi.org/10.1017/s0022463416000230.

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This article traces the evolutionary record of urbanism at two sites in Myanmar: their transition from late prehistory inc. second to first century BCE to proto-urban and fully urban development at Sri Ksetra and Beikthano by the mid-first millennium CE. The Pyu cities are remarkable because of their spatial continuity, for their early achievements in water control, iron production, ritual and domestic ceramics, brick monumental architecture, rich funerary culture, literacy and adoption of Buddhism on both elite and popular levels. Though the radiocarbon dates for Pyu urbanism are at present e

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8

Kyaing, Win. "Recent Archaeological Research at Śrīkṣetra". Journal of Burma Studies 28, № 1 (2024): 11–41. http://dx.doi.org/10.1353/jbs.2024.a923228.

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Abstract: Archaeological research on Śrīkṣetra has been ongoing for over a century, with surveying, recording, identifying monuments, excavation, and restoration. However, systematic excavation and the application of scientific measures to improve our understanding of the history and culture of the most influential and largest of the Pyu ancient cities have only lately been carried out there. Recent archaeological work by national and international scholars has introduced new ways to approach the details of Pyu urban morphology and to examine sociocultural changes, the dissemination of the ear

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9

Kircaburun, Kagan, Sabah Balta, Emrah Emirtekin, Şule Betül Tosuntas, Zsolt Demetrovics, and Mark D. Griffiths. "Compensatory Usage of the Internet: The Case of Mukbang Watching on YouTube." Psychiatry Investigation 18, no. 4 (2021): 269–76. http://dx.doi.org/10.30773/pi.2019.0340.

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Objective Accumulating empirical research has emphasized that a wide range of online activities–such as using social networking sites–can be performed in order to compensate unattained needs or to cope with negative affect and psychopathological symptoms. Although the correlates of problematic social networking use have been extensively investigated, less is known about problematic YouTube use (PYU), an umbrella term grouping a number of different activities (e.g., viewing of online video games, watching specific YouTube channels). Furthermore, nothing is known concerning increasingly popular

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10

Boisvert, Mathieu. "A Socio-cultural Analysis of the Burmese Shin pyu Ceremony." Journal of Beliefs & Values 21, no. 2 (2000): 203–11. http://dx.doi.org/10.1080/713675499.

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11

Hudson, Bob. "Funerary Practices at Pyu Sites in Myanmar and the Appearance of Buddhist Artifacts from the Fifth to Sixth Century CE Period." Journal of Burma Studies 28, no. 1 (2024): 141–67. http://dx.doi.org/10.1353/jbs.2024.a923232.

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Abstract: An ongoing research question in Myanmar (Burma) is to what extent, and in what specific part of the first millennium CE, traces of Buddhism from India can be observed in the early urban “Pyu” culture. Burial urns feature significantly in the archaeological record, but they do not have any specifically Buddhist features. Some funerary shrines feature a brick plinth at one end. If these were bases for stūpas or Buddha images, then Indian influence could be attributed as early as the second–third century CE period. No evidence has yet been found of what these plinths carried. A later bu

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12

Zhang, Mengmeng, Junfeng Shen, Chenglu Li, et al. "Genesis of the Sanhetun Tellurium–Gold Deposit, Northeast China: Constraints from In Situ Elemental and Sulfur Isotopic Compositions of Pyrite." Minerals 14, no. 10 (2024): 1014. http://dx.doi.org/10.3390/min14101014.

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The Sanhetun tellurium–gold (Te–Au) deposit, located in the Duobaoshan polymetallic metallogenic belt (DPMB) within the eastern section of the Central Asian Orogenic Belt (CAOB), is a newly discovered small-scale gold deposit. The mineralization, with a resource of ≥4 t Au, is mainly hosted in three NNE-trending alteration zones between Early Carboniferous granitic mylonite and Lower Cretaceous volcanogenic-sedimentary formations. The genesis of formation of this deposit is poorly constrained. Here, we report the results of petrographic studies, TESCAN Integrated Mineral Analyzer (TIMA), major

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13

Aktar, Taslima. "Political Dynamics of Pre-colonial Myanmar/ Burma: The Context for Colonisation." Indian Historical Review 51, no. 2 (2024): 222–37. http://dx.doi.org/10.1177/03769836241287054.

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In Burmese historiography, the issue of periodisation has not been given much attention. Burma’s pre-colonial history of dynastic and ruler changes occurred within a static framework with little to no institutional or social change. Before the British conquest, the political history of Burma can be summed up as an endless struggle between the Burmese people and their neighbours, as well as between at least four different indigenous groups: Shans, Arakanese, Mons or Talaings. Numerous political organisations and migrations occurred during the pre-colonial era. The Pyu city-states, the Pagan Emp

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14

Song, Weifang, Pan Wu, Jianzhong Liu, et al. "Genesis of the Tangshang Au Deposit in Southeast Yunnan Province, China: Constraints from In Situ Chemical and S-Sr Isotope Analyses." Minerals 12, no. 7 (2022): 806. http://dx.doi.org/10.3390/min12070806.

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The Yunnan–Guizhou–Guangxi district (also known as the Dian–Qian–Gui “Golden Triangle”) in southwestern China contains numerous Carlin-type Au deposits (CTGDs). However, the sources of Au and Au-bearing fluids in these deposits remain controversial. The Tangshang Au deposit is a middle-sized CTGD in southeastern Yunnan Province. This study involved in situ chemical and S isotope analyses of sulfides and in situ trace elemental and Sr isotope analyses of ore-related calcite; these data were used to trace the sources of fluids and Au, as well as the genesis of this deposit. Four pyrite types (Py

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15

Pyun, Danielle O., and Kyung-Eun Yoon. "Discourse functions of Korean ‘yes’ words." Korean Linguistics 18, no. 1 (2022): 48–75. http://dx.doi.org/10.1075/kl.00013.pyu.

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Abstract This study examines discourse functions of Korean ‘yes’ words from an interactional perspective based on naturally-occurring conversation data. Tokens of yey, ney, ey, ung, um, and e in Korean are widely recognized as affirmative responses. A close examination of these tokens, however, reveals wide-ranging interactional functions through which speakers express active engagement, share information, negotiate meaning, and maintain discourse coherence. The present study identifies a total of fifteen discourse-pragmatic functions of Korean ‘yes’ words: (1) affirmative answer, (2) confirma

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16

Boisvert, Mathieu. "La cérémonie de l'ordination mineure bouddhique (shin pyu) en Birmanie et ses ramifications sociales." Studies in Religion/Sciences Religieuses 30, no. 2 (2001): 131–49. http://dx.doi.org/10.1177/000842980103000201.

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Cet article est le résultat d'une étude sur les moinillons de la tradition theravāda birmane que nous avons effectuée au printemps 1999. Dans les pages qui vont suivre, nous analyserons l'admission temporaire de jeunes garçons au sein de l'ordre monastique bouddhique, ainsi que la cérémonie rituelle qui vient encadrer cet acte important. Cette étude nous permet également d'entrevoir le rôle éducatif que les monastères birmans (kyaung) entretenaient, d'examiner comment certains de ceux-ci se sont transformés en prahita pour accueillir les enfants ne pouvant se permettre financièrement de fréque

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17

Liljeblad, Jonathan. "The Pyu Ancient Cities World Heritage application: lessons from Myanmar on transnational advocacy networks." Journal of Civil Society 13, no. 1 (2016): 18–34. http://dx.doi.org/10.1080/17448689.2016.1246138.

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18

Mi, Mi Hlaing. "Achievement of Ancient Myanmar Kings for Irrigation System." Bago University Research Journal Vol. 8, No. 1, no. 2018 (2018): 68–70. https://doi.org/10.5281/zenodo.3918861.

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When ancient Pyu cities came into existence before King Anawrahta ascended the throne, it was discovered that they had built reservoirs and lakes and made arrangements to obtain regular supply of water for cultivation of crops, by digging canals. Pyus also initiated to employ methods of cultivation by irrigated water along the basin of river Ayeyawady and flooded plain land area. Beikthano, Sriksetra and Kyaukse were congested with the ancient weirs, constructed by ancient Myanmar kings. Although system of cultivation with irrigated water seemed to be an old system, it was very systematic.

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19

Song, Fanyue, Qianhui Zhang, Kadio Aka Donald Koua, et al. "Trace Element and Sulfur Isotopic Analysis of Pyrite from the Luyuangou Gold Deposit, Xiong’ershan Au-Ag Polymetallic District, Central China: Implications for The Origin and Evolution of Ore-Forming Fluids." Minerals 13, no. 3 (2023): 407. http://dx.doi.org/10.3390/min13030407.

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The Luyuangou gold deposit is located in the eastern section of the Xiong’ershan Au-Ag polymetallic district (XESPMD) and consists of a few gold-bearing veins found in the EW-striking faults located in the Archean Taihua and Mesoproterozoic Xiong’er Groups. The gold deposits contain numerous gold-bearing pyrites in thin quartz veins, representing an ideal tool for explaining the enigmatic genesis of gold deposits in the XESPMD. The distributions of trace elements and the sulfur isotopes of gold-bearing pyrite in the Luyuangou gold deposit were investigated to define the origin and evolution of

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20

Miles, James, Marc Miyake, and Nathan W. Hill. "The use of Reflectance Transformation Imaging in the recording and analyses of Burmese Pyu inscriptions." Archaeological Research in Asia 16 (December 2018): 130–38. http://dx.doi.org/10.1016/j.ara.2018.09.001.

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21

Dr., Thidar Aung. "Min Thu Won ei Nga Kapyar Myar Ma Tin Pyu Yay Phwe Han Laylar Chat." Dagon University Research Journal Vol.8, no. 2018 (2019): Pg.27–46. https://doi.org/10.5281/zenodo.3554880.

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22

O'Connor, Richard A. "Agricultural Change and Ethnic Succession in Southeast Asian States: A Case for Regional Anthropology." Journal of Asian Studies 54, no. 4 (1995): 968–96. http://dx.doi.org/10.2307/2059956.

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In the first millennium A.D. mainland Southeast Asia's first great states arise, but then in the span of a few centuries these Indianized realms collapse and their Pyu, Mon, Khmer, and Cham peoples decline. In their place Burmese, Tai, and Vietnamese states arise and go on to rule the mainland as their peoples come to dominate the second millennium. Case by case these shifts appear to be ethnic and political successions wherein the strong displace the weak, but seen together regionally the similarities suggest an agricultural change whereby an irrigated wet rice specialization from upland vall

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23

Wang, Cheng, Yongjun Shao, Kuanxin Huang, et al. "Ore-Forming Processes at the Xiajinbao Gold Deposit in Eastern Hebei Province: Constraints from EPMA and LA-ICPMS Analysis." Minerals 8, no. 9 (2018): 388. http://dx.doi.org/10.3390/min8090388.

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The Xiajinbao gold deposit is located at the northern margin of the North China Craton. Hydrothermal pyrites belonging to three stages were identified: Py1; Py2; and Py3. Geochemical study of these pyrites was conducted using electron probe microanalysis and laser ablation inductively coupled plasma mass spectrometry to investigate the distributions of minor and trace elements, constrain pyrite genesis, and to obtain an improved understanding of the ore-forming processes. Py1 and Py2 contain high concentrations of Au and are interpreted to have been deposited from fluids from a dominantly magm

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24

Deeg, Max. "Chinese Reports about Buddhism in Early Burma." Journal of Burma Studies 28, no. 1 (2024): 125–40. http://dx.doi.org/10.1353/jbs.2024.a923231.

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Abstract: This article revisits the Chinese Buddhist sources on the Pyus and Śrīkṣetra in early Burma. Buddhist references to the region mainly come from the Tang period (618–907). These texts, authored by the famous monks Xuanzang and Yijing, do not use the Chinese transcriptional term Biao, which corresponds to Pyu, but exclusively use the name Śrīkṣetra. They do not refer to any local form of Buddhism or do so only in very general terms. Buddhism as practiced by the Pyus (Biao) is first mentioned in the ninth-century text, the Manshu . The Chinese sources certainly do not prove that Buddhis

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25

Zhang, Zhichao, Yuwang Wang, Jiyu He, et al. "Geology, Pyrite Geochemistry and Metallogenic Mechanism of the Wulong Gold Deposit in Liaodong Peninsula, North China Craton." Minerals 12, no. 12 (2022): 1551. http://dx.doi.org/10.3390/min12121551.

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The Wulong deposit is a large gold deposit in the Liaodong peninsula (North China Craton). Silicic and pyrite alterations are well-developed in the deposit and closely related to mineralization. The least altered and silicified microdiorite samples were selected for major and trace element analyses to reveal the elemental migration/enrichment. Pyrites of stage 1 (Py1) were selected for backscattered electron (BSE) imaging and LA-ICP-MS trace element analyses to reveal their possible metallogenic link. Mass balance calculation showed that Al2O3, CaO, Fe2O3, K2O, SiO2, Ag, As, Cu, and Pb were br

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26

Hidayat, Muhammad Rizyan Anggra, F. X. Wagiman, and Arman Wijonarko. "Arthropod Diversity in the Tea Plantation within Several Years after Pruning in Pagilaran, Central Java." Jurnal Perlindungan Tanaman Indonesia 23, no. 2 (2019): 299. http://dx.doi.org/10.22146/jpti.47172.

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The lush leaves of tea within several years after prune is expected to be followed by arthropod abundance and diversity. The study aimed to evaluate the arthropod abundance, diversity, evenness, and dominance, at the tea plantation within several years after the prune. The study was conducted at Pagilaran tea plantations, Central Java, from April to May 2018, at an altitude of 900 m asl. Arthropod samplings were done in four plots of tea plantation namely 1, 2, 3, and 4 years after pruning, hereafter they are called PY1, PY2, PY3, and PY4. The plot area was approximately 1 ha. The arthropod sp

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27

Chan Ko Ko, Aye, Zhang Ying, and Theint Theint Htun. "Study on Socioeconomic Impacts of Private Forest Plantations on Local Livelihood in Pyu Township, Taungoo District, Bago Region, Myanmar." International Journal of Sciences 3, no. 02 (2017): 43–54. http://dx.doi.org/10.18483/ijsci.1193.

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28

Chan, Ko Ko Aye, Zhang Ying, and Htun Theint Theint. "Study on Socioeconomic Impacts of Private Forest Plantations on Local Livelihood in Pyu Township, Taungoo District, Bago Region, Myanmar." International Journal of Sciences Volume 6, no. 2017-02 (2017): 43–54. https://doi.org/10.5281/zenodo.3349365.

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Forest Department of Myanmar has called for private investment in plantation forestry by granting forest land concession right since 2006-07. On the other hand, rural peoples of the country, representing about 70% of total population, rely on forest resources and forest land for their livelihood. This paper explores the socio-economic impacts of private forest plantations on rural communities in Pyu Township, Taungoo district, Bago Region, Myanmar. According to our results private forest plantations have the potential to positively impact on local people's wealth and well-being, if enough emph

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29

Wicks, Robert S. "The Ancient Coinage of Mainland Southeast Asia." Journal of Southeast Asian Studies 16, no. 2 (1985): 195–225. http://dx.doi.org/10.1017/s0022463400008419.

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Southeast Asia's coinage during the first millenium AD is remarkably conservative and uniform. A single prototype, a silver conch and śrīvatsa coin, is the model for each mainland coinage issued over a period of more than five hundred years, from about AD 450 to 1000. (Plate 1, coin 1) Silver is by far the preferred metal for minting. Gold and copper are rarely used, and then only in late or debased issues. Most of the cointypes are limited in circulation to their place of issue, providing insight into the geographical extent of effective political control in the early states of Candra Arakan,

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30

Kurz, Johannes L. "Piaoyue, Piao, Pyu (?): Chinese Textual Evidence Concerning a Southeast Asian Region in Burma from the Tang to the Song Dynasties." Journal of Asian History 58, no. 1-2 (2024): 89–115. https://doi.org/10.13173/jah.58.1-2.089.

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31

Bronson, Bennet. "Burma - The Ancient Pyu of Burma. Vol. 1: Early Pyu Cities in a Man-Made Landscape. By Janice Stargardt. Cambridge: Publications on Ancient Civilization in South East Asia and Singapore: Institute of Southeast Asian Studies, 1990. Pp. xxix, 416. Illustrations, Maps, Notes, Bibliography, Index." Journal of Southeast Asian Studies 23, no. 2 (1992): 435–38. http://dx.doi.org/10.1017/s0022463400006342.

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32

Bouihi, Fatiha, Bruno Schmaltz, Fabrice Mathevet та ін. "D-π-A-Type Pyrazolo[1,5-a]pyrimidine-Based Hole-Transporting Materials for Perovskite Solar Cells: Effect of the Functionalization Position". Materials 15, № 22 (2022): 7992. http://dx.doi.org/10.3390/ma15227992.

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Donor–acceptor (D–A) small molecules are regarded as promising hole-transporting materials for perovskite solar cells (PSCs) due to their tunable optoelectronic properties. This paper reports the design, synthesis and characterization of three novel isomeric D-π-A small molecules PY1, PY2 and PY3. The chemical structures of the molecules consist of a pyrazolo[1,5-a]pyrimidine acceptor core functionalized with one 3,6-bis(4,4′-dimethoxydiphenylamino)carbazole (3,6-CzDMPA) donor moiety via a phenyl π-spacer at the 3, 5 and 7 positions, respectively. The isolated compounds possess suitable energy

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33

Yu, Qi, Zhigao Wang, Qingfei Sun, and Keyong Wang. "In Situ Trace Element and Sulfur Isotope Composition of Pyrite from the Beiwagou Pb-Zn Deposit, Liaodong Peninsula, Northeast China: Implications for Ore Genesis." Minerals 13, no. 9 (2023): 1176. http://dx.doi.org/10.3390/min13091176.

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The Beiwagou Pb-Zn deposit, located in the western part of the Liaodong Peninsula, is a carbonate-hosted stratiform deposit with a Pb + Zn reserve of 0.08 Mt @ 4.14% (Pb + Zn). The orebodies occur as conformable layers and lenses and are strictly controlled by strata (the Paleoproterozoic Gaojiayu and Dashiqiao Formations) and lithology (plagioclase amphibolite and dolomitic marble). Given that previous studies have focused only on the mineralization features and mineralogy of deposits, herein, we report in situ trace element analyses of pyrite using LA-ICP-MS, together with in situ sulfur iso

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34

Liu, Ji, Xinshang Bao, Yongbao Gao, et al. "Composition and Geochemical Characteristics of Pyrite and Quartz: Constraints on the Origin of the Xinjiazui Gold Deposit, Northwestern Margin of the Yangtze Block, China." Minerals 12, no. 6 (2022): 688. http://dx.doi.org/10.3390/min12060688.

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The Xinjiazui gold deposit, a newly discovered deposit, is situated in the northwestern margin of the Yangtze Block, China. The source and genesis of gold mineralization are poorly understood. It is urgent to use the H–O isotopic composition of quartz and geochemistry of pyrite to evaluate the origins of the Au and ore-forming fluids of this deposit. Three types of pyrite were identified, including synsedimentary framboidal pyrites (Py0), the directional arrangement of pyrites in pre-mineralization stage (Py1), and euhedral coarse-grain pyrites in the quartz–sulfide veins of the mineralization

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35

Saito, Isao, Yoshio Saito, Kazuo Hanawa, et al. "Highly selective fluorescent nucleobases for designing base-discriminating fluorescent probes." Pure and Applied Chemistry 78, no. 12 (2006): 2305–12. http://dx.doi.org/10.1351/pac200678122305.

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There is increasing interest in single nucleotide polymorphism (SNP) typing since they can be used as markers to identify the genes that underlie complex diseases and to realize the full potential of pharmacogenomics in analyzing variable response to drugs. Among the different methodologies for SNP genotyping, the homogenous assay is more amenable than the heterogeneous one.In this article, we will describe some of our most recently developed novel base-discriminating fluorescent (BDF) nucleosides useful for homogenous SNP typing. Our novel concept led to the investigation of a new type of pyr

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36

Tirkey, Yaswant. "गुप्तकालीन लोक, नृत्य एवं संगीत कला". International Journal of Advance and Applied Research 5, № 30 (2024): 231–34. https://doi.org/10.5281/zenodo.13960357.

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xqIrdky esa u`R;&laxhr foèkk dk cgqr fodkl gqvkA rRdkyhu le; esa olUrksRlo] dkSeqnh egksRlo] nhiksRlo vkfn ij u`R;&laxhr dk çpyu FkkA ml dky esa xf.kdkvksa dk mYys[k feyrk gS ftudk çeq[k dk;Z u`R; vkSj xk;u FkkA xqIr 'kkldksa }kjk dykdkjksa dks çJ; nsus dh tkudkjh Hkh feyrh gSA leqæxqIr Lo;a ,d Js"B oh.kkoknd Fks blfy;s viuh Le`fr dks thfor j[kus ds fy;s mUgksaus oh.kkèkkjh çdkj ds flôksa dks pyok;kA xqIrdkyhu ok?k dh xqQkvksa esa u`R;&laxhr dk ,d egÙoiw.kZ fp= feyrk gS tks rRdkyhu le; esa u`R;&laxhr ds oSHko ds ifjpk

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37

Kouhestani, Hossein, Majid Ghaderi, Peyman Afzal, and Khin Zaw. "Classification of pyrite types using fractal and stepwise factor analyses in the Chah Zard gold-silver epithermal deposit, Central Iran." Geochemistry: Exploration, Environment, Analysis 20, no. 4 (2020): 496–508. http://dx.doi.org/10.1144/geochem2020-031.

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The major target of this research is the classification of pyrite types using fractal and stepwise factor analyses in the Chah Zard ore deposit, Central Iran. The ore occurs within a breccia/vein type and the major ore mineral hosting gold mineralization is pyrite. In this study, data were selected using optical, scanning electron microscopy (SEM) and backscattered electron observations as well as laser ablation-inductively coupled plasma–mass spectrometry (LA-ICP–MS) analysis. Conventional interpretations represent four gold-bearing pyrite types of various textures including fractured and por

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38

Nan, Guizhou, Jing Xu, Wenyuan Liu, Suyu Chen, Zhihui Cen, and Jichen Jiang. "Enrichment of Se-Te-Au in the Jilongshan Au-Cu Skarn Deposit, Hubei Province: Insight from Pyrite Texture and Composition." Minerals 13, no. 12 (2023): 1516. http://dx.doi.org/10.3390/min13121516.

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Selenium and Te are two important critical metals, which are often produced as by-products in Au-Cu deposits related to magmatic–hydrothermal systems, such as porphyry and skarn deposits. The Jilongshan Au-Cu deposit is a typical skarn deposit located in the middle and lower parts of the Yangtze River metallogenic belt. Previous studies show that it has valuable Se and Te resources, but their occurrence, particularly the relationship between the texture and composition of pyrite, and the enrichment mechanism of Se, Te, and Au remain unclear. Here, the textures and the major and trace elements

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Kudrin, Maxim V., Valery Yu Fridovsky, Lena I. Polufuntikova, and Lyudmila Yu Kryuchkova. "Disseminated Gold–Sulfide Mineralization in Metasomatites of the Khangalas Deposit, Yana–Kolyma Metallogenic Belt (Northeast Russia): Analysis of the Texture, Geochemistry, and S Isotopic Composition of Pyrite and Arsenopyrite." Minerals 11, no. 4 (2021): 403. http://dx.doi.org/10.3390/min11040403.

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At the orogenic gold deposits of the Yana–Kolyma metallogenic belt (northeast Russia) both Au–quartz-sulfide mineralization with native gold and disseminated sulfide mineralization with invisible Au developed. The textural and mineralogical-geochemical features, isotope-geochemical characteristics of gold-bearing sulfides from proximal metasomatites, and possible forms of Au occurrence in pyrite and arsenopyrite have been studied using electron microprobe, atomic absorption, LA-ICP-MS trace element, isotope analysis, and computed microtomography. Four generations of pyrite (Py1, diagenetic; Py

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Zin, Monika. "Stūpa Shapes from the Āndhra Country to Śrīkṣetra". Journal of Burma Studies 28, № 1 (2024): 43–71. http://dx.doi.org/10.1353/jbs.2024.a923229.

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Abstract: Indian influence on the architecture of the Pyus is demonstrable in several instances. The shape of their city gates, for example, repeats the Indian “ lizard ’ s mouth ” ( godhāmukha ), described in the Kauṭilīya Arthaśāstra and widespread in India. The objects of art and architecture created by the Pyus do not, however, display any recognizable similarities to those of Āndhra; the style of the preserved representations of the Buddha and ornaments like the makara , even on the objects that are usually taken to be early examples, corresponds with the Gupta or even post-Gupta style (f

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Yang, Hui, and Huashan Sun. "Microfabrics, In Situ Trace Element Compositions of Pyrite, and the Sulfur Isotope Chemistry of Sulfides from the Xitieshan Pb-Zn Deposit, Qinghai Province, Northwest China: Analysis and Implications." Minerals 13, no. 12 (2023): 1549. http://dx.doi.org/10.3390/min13121549.

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The Xitieshan deposit, located in the central segment of the northern margin of the Qaidam Basin, is among the largest massive Pb-Zn sulfide deposits in China. This deposit, along with its ore-bearing rock series known as the Tanjianshan Group, underwent greenschist facies metamorphism due to subsequent orogeny. We investigated the in situ sulfur isotopes of sulfides with different occurrences to define the origin of ore-forming fluids. The δ34S values of sulfides from stratiform ores, massive ores in schist, stockwork ores in marble, schist and discolored altered rocks that constitute a typic

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Griffiths, Arlo, Bob Hudson, Marc Miyake, and Julian Wheatley. "Studies in Pyu Epigraphy, I: State of the Field, Edition and Analysis of the Kan Wet Khaung Mound Inscription, and Inventory of the Corpus." Bulletin de l'Ecole française d'Extrême-Orient 103, no. 1 (2017): 43–205. http://dx.doi.org/10.3406/befeo.2017.6247.

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Liljeblad, Jonathan, and Khin Thinn Thinn Oo. "World heritage sustainable development policy & local implementation: Site management issues using a case study of Sri Ksetra at Pyu ancient cities in Myanmar." Sustainable Development 28, no. 3 (2020): 468–77. http://dx.doi.org/10.1002/sd.2037.

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Sundarrajan, Vijay Anand, Carolin Nicole Marjon, and Baba Musta. "Micron to Nano Au Particles Incorporation in Different Stages of Pyrite, in Bau, Sarawak, Malaysia." Indonesian Journal on Geoscience 12, no. 1 (2025): 89–103. https://doi.org/10.17014/ijog.12.1.89-103.

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In eastern Malaysia, Bau is the significant sediment hosted gold deposit (SHG), and Sarawak Province was the main gold (Au) producer in East Malaysia. The annual production rate was approximately 40 ̶ 50 metric tons of Au (high grade). The Bau mining is located 40 km SW of Kuching City, Sarawak. For the present study, around twenty-five samples were collected in the Au mineralized zones of Bau areas. The polished thin sections were prepared for mineral chemistry and fluid petrography analyses. The samples were studied through transmission microscope, Electron Probe Micro-Analyzer (EPMA), and f

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Wang, Ying, Ke Shi, Ze Zhong, et al. "Rb–Sr Pyrite Dating and S–Pb Isotopes in the Fang’an Gold Deposit, Wuhe Area, Eastern Anhui Province." Minerals 14, no. 4 (2024): 398. http://dx.doi.org/10.3390/min14040398.

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The Fang’an gold deposit in the Wuhe area, Anhui Province, is located in the area adjacent to the Bengbu Uplift and Wuhe Platform Depression in the southeastern part of North China. This study aimed to determine the deposit’s mineralization age and the source of its metallogenic materials and mineralization processes through investigations into its geological characteristics, Rb–Sr isotopes, and S–Pb isotopes. The orebodies of the Fang’an gold deposit in the Neoarchean Xigudui Formation primarily exhibit a vein-type structure. The ore-forming process can be divided into four stages: (i) the qu

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Peng, Hong-Wei, Hong-Rui Fan, Xuan Liu, Bo-Jie Wen, Yong-Wen Zhang, and Kai Feng. "New Insights Into the Control of Visible Gold Fineness and Deposition: A Case Study of the Sanshandao Gold Deposit, Jiaodong, China." American Mineralogist 106, no. 1 (2021): 135–49. http://dx.doi.org/10.2138/am-2020-7475.

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Abstract Mineralogical distribution, textures, electron probe microanalysis of visible gold, laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) trace element analysis of pyrite, and LA-multicollector (MC-)ICP-MS sulfur isotope analysis of sulfide minerals are examined in an ore zone extending obliquely to –4 km depth in the Sanshandao gold deposit Jiaodong, China. We relate these results to the temporal and spatial ore-forming processes in the deposit to further elucidate the controls on the deposition of visible Au and fineness variation. Two generations of Au mineralizat

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Sutkin, A. V., O. P. Vinkovskaya, and A. S. Krasnopevtseva. "Alien plants of the flora of Baikal Siberia - updating floristic data." Проблемы ботаники Южной Сибири и Монголии 22, no. 1 (2023): 360–63. http://dx.doi.org/10.14258/pbssm.2023069.

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Information about composition of the alien fraction of the flora of Baikal Siberia (BS) is given, which includes 465 species and subspecies of alien plants belonging to 282 genera and 70 families. At the same time, the same number of alien species were noted in the Irkutsk region (IO) as in the Republic of Buryatia (RB) and Zabaikalsky krai (ZK) combined. Alien plants are extremely unevenly distributed over the territory of the BS, in some areas (the north of the RB and ZK) information on the location of adventitious species is completely absent. In terms of the number of recorded adventitious

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Nyunt, Nyunt Shwe. "The Social Life of Bagan Period." Dagon University Research Journal Vol.3, no. 2011 (2019): Pg.27–31. https://doi.org/10.5281/zenodo.3542326.

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The City Arimaddanapura, 'the City of the Enemy Crusher', or Tampadipa 'the Land of Copper', some of the original names of the old Bagan used in the lithic inscriptions. In command of the Ayeyarwady River, sited just a few miles downstream from the great tributary the Chindwin, that flows down from India and Assam. Bagan stood midway between the delta trading ports of the Mons and the China road, between the river land overland routes to India, and the scattered trails that still weave through the hills to the east, to the remainder of South East Asia. Bagan was the crossroads

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Li, Chang-Ping, Jun-Feng Shen, Sheng-Rong Li, Yuan Liu, and Fu-Xing Liu. "In–Situ LA-ICP-MS Trace Elements Analysis of Pyrite and the Physicochemical Conditions of Telluride Formation at the Baiyun Gold Deposit, North East China: Implications for Gold Distribution and Deposition." Minerals 9, no. 2 (2019): 129. http://dx.doi.org/10.3390/min9020129.

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The Baiyun gold deposit is located in the northeastern North China Craton (NCC) where major ore types include Si-K altered rock and auriferous quartz veins. Sulfide minerals are dominated by pyrite, with minor amounts of chalcopyrite, sphalerite and galena. Combined petrological observations, backscattered electron image (BSE) and laser ablation analysis (LA-ICP-MS) have been conducted on pyrite to reveal its textural and compositional evolution. Three generations of pyrite can be identified—Py1, Py2 and Py3 from early to late. The coarse-grained, porous and euhedral to subhedral Py1 (mostly 2

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Norman, K. R. "The ancient Pyu of Burma. Volume one. Early Pyu cities in a man-made landscape. By Janice Stargardt. pp. xxix, 416, 135 figs. 16 pl., 3 aerial photographs of sites and 3 associated archaeological maps in pocket. Cambridge, Publications on Ancient Civilisations in South East Asia (PACSEA) in association with the Institute of Southeast Asian Studies (ISEAS) Singapore, 1990. £47.00 (cloth), £27.00 (paperback)." Journal of the Royal Asiatic Society 2, no. 1 (1992): 114–17. http://dx.doi.org/10.1017/s1356186300002170.

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