Chapter 9 Palaeoarchaean–Mesoproterozoic sedimentation and tectonics along the west-northwestern margin of the Singhbhum Granite body, eastern India: a synthesis

10.1144/m43.9 ◽  
2015 ◽  
Vol 43 (1) ◽  
pp. 121-138 ◽  
Author(s):  
Gautam Ghosh ◽  
Bhaskar Ghosh ◽  
Joydip Mukhopadhyay
Author(s):  
Bihani Sarkar

Fundamental in making the myth of civilization meaningful in Indian culture was the performance of the Navarātra, the festival of the Nine Nights, which was intertwined with Durgā's cult. This final chapter deals with how the cult functioned in creating the spectacle of ‘public religion’ through a reconstruction of this ritual in which the goddess was worshipped by a ruler in the month of Āśvina. A detailed exposition of the modus operandi of the Nine Nights shows us how the religion of the goddess was spectacularly brought to life in an event of grand theatre and solemnized before its participants, the king and the entire community. The development of the Nine Nights from a fringe, Vaiṣṇava ceremony in the month of Kṛṣṇa's birth under the Guptas, to a ritual supplanting the established autumnal Brahmanical ceremonies of kingship and finally into a crucial rite in Indian culture for consolidating royal power, formed a crucial motivation for the expansion of Durgā's cult. The chapter isolates and analyzes in depth the principal early traditions of the Navarātra in East India and in the Deccan by an assessment of the available ritual descriptions and prescriptions in Sanskrit and eye-witness sources from a later period, used to fill in the gaps in the earlier sources. The most elaborate description of a court-sponsored rite emerges from the Kārṇāṭa and Oinwar courts of Mithilā, which embody what appears to be a ritual that had matured a good few centuries earlier before it was recorded in official literature. Among these the account of the Oinwars by the Maithila paṇḍita Vidyāpati is the most extensive treatment of the goddess's autumnal worship by a king, and attained great renown among the learned at the time as an authoritative source. His description portrays a spectacular court ceremony, involving pomp and pageantry, in which horses and weapons were worshipped, the king was anointed, and the goddess propitiated as the central symbol of royal power in various substrates over the course of the Nine Nights. Vidyapati's work also reveals the marked impact of Tantricism on the character of the rite, which employed Śākta mantras and propitiated autonomous, ferocious forms of the goddess associated with the occult, particularly on the penultimate days. Maturing in eastern India, the goddess's Navarātra ceremony was proselytized by the smartas further to the west and percolated into the Deccan, where, from around the 12th century, it attained an independent southern character. Whereas the eastern rite focused on the goddess as the central object of devotion, the southern rite focused on the symbolism of the king, attaining its most distinctive and lavish manifestation in the kingdom of Vijayanagara. Throughout this development, the Navarātra remained intimately associated with the theme of dispelling calamities, thereby augmenting secular power in the world, sustaining the power of the ruler and granting political might and health to a community. It remained from its ancient core a ritual of dealing with and averting crises performed collectively by a polis. Such remains its character even today.


Food Security ◽  
2022 ◽  
Author(s):  
Dileep Kumar Pandey ◽  
Kalkame Ch Momin ◽  
Shantanu Kumar Dubey ◽  
Poovaragavalu Adhiguru

2015 ◽  
Vol 8 (10) ◽  
pp. 8703-8719 ◽  
Author(s):  
Dmitry Anatolievich Novikov ◽  
Anna Fedorovna Sukhorukova

1957 ◽  
Vol 20 (1) ◽  
pp. 159-166
Author(s):  
Anthony Christie

It is now more than 50 years since Paul Pelliot studied, in Deux ītinéraires de Chine en Inde, a work which, together with Le Fou-nan, laid the foundations for much of the subsequent development of South East Asian studies, certain itineraries between China and the West. These itineraries had been compiled by Chia Tan (A.D. 730–805) and date from the period A.D. 785–805, but, the original compilation having been lost, they are extant only in the summaries preserved in the Hsin T‘ang shu. Among the routes included is one from Yunnan to India which crosses Upper Burma by alternative ways, bifurcating at Chu-ko Liang and rejoining in Eastern India whence it leads to Magadha.


1989 ◽  
Vol 126 (4) ◽  
pp. 363-372 ◽  
Author(s):  
Wes Gibbons

AbstractOn mainland North Wales basement rocks emerge from beneath a Lower Ordovician cover along the west side of the Llyn peninsula. The basement contains steeply dipping mylonites (Llŷn shear zone) that separate plutonic and gneissic rocks (Sarn Complex) from a melange (Gwna mélange). The western edge of the Ordovician outcrop follows the basement shear zone, and new trenching data confirm that only a faulted relationship exists between cover and basement along this northwestern extremity of the Welsh Basin. Deformation along this margin has propagated into the Arenig cover to produce southeasterly verging thrusts, asymmetric folds and northwesterly dipping cleavage. A prominent steep fault (Daron Fault) cutting the Ordovician succession follows an eastern splay of the Llŷn shear zone and again therefore records brittle reactivation of an underlying mylonite belt. The likelihood of syn-Arenig fault movements is provided by the presence of a prominent late Arenig coarse clastic unit, containing boulders of the basement mylonites, that is found only to the west of the Daron Fault. Steep basement structures such as the Llŷn shear zone, initially generated as major transcurrent faults, are interpreted as having exerted a strong control over the deposition and subsequent deformation of the Ordovician cover sequence.


2011 ◽  
Vol 149 (4) ◽  
pp. 578-589 ◽  
Author(s):  
G. M. YOUNG ◽  
W. G. E. CALDWELL

AbstractTwo strikingly different successions of Lower Carboniferous (mainly Tournaisian) sedimentary rocks are closely juxtaposed on the NE coast of the island of Arran, SW Scotland. Near the village of Corrie a thin succession (~ 17 m) of Tournaisian rocks is preserved, whereas in the neighbouring Fallen Rocks–Laggan area, correlative rocks are > 300 m in thickness. These contrasting successions are separated by the Laggan Fault, which is a landward extension of the submarine Brodick Bay Fault, marking the SW boundary of the Northeast Arran Trough. The contrasting thickness and stratigraphy of the two sequences of sedimentary rocks result from juxtaposition of shoulder and trough deposits along the Laggan–Brodick Bay Fault. Although originally a normal, basin-defining fault, later sinistral movements caused significant displacement of the NE Arran Trough, together with a segment of the Highland Boundary Fault, from their original positions. The most northerly occurrence of the Highland Boundary Fault on Arran is thought to be the truncated northern end of the Corloch Fault. To the SW the surface trace of the Highland Boundary Fault is largely obscured by a Palaeogene granite body but it is present on the west side of the island, near Dougrie. The Highland Boundary Fault appears to be displaced to the south, in Kilbrannan Sound, by a series of NW-trending sinistral transcurrent faults. Thus the ‘anomalous’ trend of the Highland Boundary Fault and narrowing of the Midland Valley of Scotland in the Firth of Clyde area may be explained by later fault movements and intrusion of the Palaeogene North Arran Granite Pluton.


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