ABSTRAK Penelitian berjudul “ Kajian Tekstur Dramatik Lakon Mintaraga Sajian Wayang Wong Sriwedari” merupakan penelitian kualitatif dengan cara melihat pertunjukan dan menganalisis menggunakan teori ...Tekstual. Teori ini dikemukakan oleh Satoto yang mengungkapkan bahwa tekstur dramatik adalah sesuatu yang terindera. Hasil penelitan ini mengungkap berbagai elemen pertunjukan meliputi dialog, iringan musik dan spektakel. Dialog dapat didengar pilah atau tidaknya yang disesuaikan dengan karakter tokoh yang dimainkan, iringan musik dapat didengar dan dikaji mengenai keselarasan dengan adegan yang dimainkan sedangkan spektakel dapat dilihat dengan indera penglihatan mengenai bentuk setting, properti dan tata cahaya yang digunakan dalam pertunjukan Wayang Wong Sriwedari Lakon Mintaraga. Kata kunci: Tekstur dramatik, Dialog, Spektakel. ABSTRAKThe research entitled “Kajian Tekstur Dramatik Lakon Mintaraga Sajian Wayang Wong Sriwedari” is a qualitative research by looking at performances and analyzing using Textual theory. This theory was put forward by Satoto. It says that dramatic texture is something that is sensed. The results of this research reveal the various elements of the show including dialogue, musical accompaniment and spectacles. Dialogue can be heard according to the characters being played, musical accompaniment can be heard and studied in harmony with the scene played, while the spectacle can be seen regarding to the form of setting, properties and lighting used in the Wayong Wong Sriwedari performance lakon Mintaraga . Keywords: Dramatic Texture, Dialogue, Spectacles.
•The Spektakel Suite consists of 22 varieties of late- to post-tectonic porphyritic granite and charnockite•The Spektakel Suite intruded the granulitic core of the Bushmanland Subprovince (BSP) ...between 1097 and 1033 Ma•The timing of termination of main penetrative deformation in the BSP is constrained to between 1109 Ma and 1097 Ma•The Spektakel Suite temporally and spatially associated with peak low-P, high-T metamorphism in the BSP (∼1050–1020 Ma)
The Spektakel Suite comprises voluminous late- to post-tectonic granitoids that intruded the pre-tectonic gneisses of the Bushmanland Subprovince (BSP) of the Mesoproterozoic Namaqua-Natal Metamorphic Province (NNMP). Based on new U-Pb zircon geochronology and geochemical data, we redefine the suite as consisting of 22 plutons of porphyritic monzogranite, granodiorite and charnockite that intruded the granulitic core of the BSP between 1097 and 1033 Ma. The new data show that some granites previously incorporated into the Spektakel Suite should be excluded: a) garnetiferous leucogranites (Concordia, Hangsfontein and Ibequas Granites) are excluded on petrological grounds and genetic considerations and b) the porphyritic Nuwefontein Granite (∼783 Ma) is younger and is now placed within the Richtersveld Suite. The Spektakel Suite has geochemical and isotopic compositions suggesting that it was derived from recycled Palaeoproterozoic crust with Mesoproterozoic mantle input. The main Namaqua Orogeny (D2) in the BSP comprises at least two phases of compressional tectonics at ∼1200 Ma and ∼1110 Ma separated by a period of extension. The new ages for the Spektakel Suite tightly constrain the end of D2 to between 1109 Ma, the age of the youngest pre-tectonic gneiss and 1097 Ma, the age of the oldest Spektakel Suite granite. Peak low-P, high-T metamorphism (∼1050–1020 Ma) occurred well after D2 and its close spatial and temporal relationship to the Spektakel Suite suggests this prolonged period of granite magmatism was responsible for the transfer of the heat into the BSP. Several other late- to post-tectonic megacrystic granitic suites intruded into other tectonic domains across the NNMP coevally with the Spektakel Suite, indicating widespread granite magmatism at this time, probably due to mafic under- and intra-plating in a back-arc setting as previously suggested.
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GEOZS, IJS, IMTLJ, KILJ, KISLJ, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, UL, UM, UPCLJ, UPUK, ZRSKP
Was sich 2015 ereignete, war kein voraussetzungsloses, plötzliches Erscheinen und keine Krise der Migration, sondern eine Krise des europäischen Grenzregimes. Neben den eigensinnigen und ...widerständigen Bewegungen der Migration war diese Zeit gekennzeichnet von zivilem Engagement und von zahlreichen Kunst- und Kulturproduktionen mit, für und über Geflüchtete. Nanna Heidenreich fragt ausgehend vom ›langen Sommer der Migration‹ nach dem Verhältnis von Hype zu Möglichkeitsraum: Wann wird Kunst mit Migration zum Spektakel? Wie stehen ästhetische Schwellenerfahrungen zum Anspruch auf politische Transformation? Auf welche Weise sind Klimawandel und Migration miteinander verschaltet, von wessen Zukunft reden wir? Und welche Farbe hat das Meer?
Aluminous metapelitic granulites from the central Namaqua Sector of the Namaqua–Natal Metamorphic Province, South Africa, host partly retrogressed hercynite–quartz assemblages. These assemblages ...record peak P–T conditions of 860–890 °C and 5–5.5 kbar, estimated via thermodynamic modelling and ternary feldspar thermometry. In-situ U–Pb geochronology and geochemistry of anatectic zircon and monazite constrains this event as part of the main Namaqua Orogeny affecting the terrane at c. 1040–1035 Ma. Detrital zircon age spectra span from about 1860 to 1100 Ma, peaking at c. 1800–1700 and 1400–1300 Ma, suggesting detritus was sourced from nearby Paleoproterozoic- and Mesoproterozoic terranes. Thin sections reveal narrow monomineralic coronae of garnet, cordierite or sillimanite separating formerly coexisting hercynite and quartz. Calculated chemical potential relationships show that coronae have developed in response to very minor, near-isobaric cooling shortly after the thermal peak, involving limited diffusion down gradients of μFeO–μMgO. Corona formation occurred in distinct compositional domains, controlled by neighbouring porphyroblasts such as garnet and/or sillimanite. Isolated hercynite–quartz pairs distal from porphyroblasts developed thin rinds of sillimanite, requiring no additional compositional gradients. Cordierite inclusions in garnet, limited melt production and extraction and corona-textures are consistent with an anticlockwise evolution, involving burial and concomitant heating to near-ultrahigh temperature conditions followed by near-isobaric cooling at mid-crustal depths. The hercynite–quartz equilibria record the highest metamorphic temperature affecting the Namaqua Sector, requiring a crucial component of advective heating via voluminous pre- to syn-metamorphic felsic-charnockitic magmatism of the Spektakel Suite. Namaqua-aged granulite facies metamorphism at the terrane scale was driven by a combination of mafic underplating and radiogenic heating. Calculated temperature–enthalpy profiles suggest that advective heating locally increased the suprasolidus enthalpy budget by a third which allowed peak temperatures to be some 50 °C higher than would otherwise have been achieved.
•Partially retrogressed hercynite–quartz-bearing metapelitic granulites from the central Bushmanland Subprovince, Namaqua–Natal Metamorphic Province (South Africa) are investigated.•Pseudosection modelling, ternary feldspar thermometry and chemical potential relationships constraint upper-granulite facies conditions of 860–890 °C at 5–5.5 kbar and an anticlockwise P–T path.•Zircon- and monazite U–Pb geochronology yields 1040–1035 Ma for peak metamorphism and detrital zircon age spectra spanning over 1860–1100 Ma.•Pre- to syn-metamorphic felsic intrusions of the Spektakel Suite contributed additional advective heat that drove metamorphism.•Calculated temperature–enthalpy relations suggest that, without this advective heat, near-ultrahigh temperatures would not have been achieved.
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GEOZS, IJS, IMTLJ, KILJ, KISLJ, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, UILJ, UL, UM, UPCLJ, UPUK, ZAGLJ, ZRSKP
A network of monazite-rich, coarse-grained veins and fine-grained veins permeating the mid-Proterozoic Concordia Granite in the Kliphoog area near Springbok, Namaqualand, North Cape Province, South ...Africa, are described with respect to their whole-rock chemistry, petrography, mineralogy, and mineral chemistry along with zircon and monazite geochronology. Chondrite-normalized trace element data indicate that the coarse-grained veins are enriched in LREE relative to the Concordia Granite with HREE enrichment being somewhat variable. HREE in altered Concordia Granite, at the contact with the coarse-grained vein, are heavily depleted compared to unaltered Concordia Granite while the LREE show the same approximate abundances. Chloritization is common in the coarse-grained veins along mineral grain boundaries with chlorite replacing most of the orthopyroxene megacrysts, though occasional remnants of orthopyroxene remain in the core. A traverse across one of the coarse-grained veins showed no obvious mineral chemical trends between the vein and surrounding granite. Relic Fe-rich megacryst orthopyroxene has an Al2O3 content of around 2.0 wt% suggesting formation at around 700 °C. The Fe-rich biotite has mean Ti values ranging from TiO2 = 4.1 to 1.2 wt% indicating formation at 700–800 °C. The coarse-grained veins and fine-grained veins are characterized by abundant accessory Th-rich monazite, heterogeneously distributed in the veins. Lesser amounts of monazite are found in the granite. Other accessory minerals in the veins and granite include zircon and rare fluorapatite. Back-scattered electron imaging shows that the anhedral to euhedral monazite grains (up to more than 1500 μm in size) tend to be complexly zoned with light and dark areas. Lighter areas are more enriched in Th and/or Ce than darker areas. This complex zoning can occur as magmatic/sector zoning and more commonly as a complex series of metasomatic alteration events. Metasomatic textures, which are due to variable fluid-induced mobility of Th, U, and REE, are the result of a coupled dissolution-reprecipitation process and have been reproduced experimentally using high pH alkali-bearing fluids. The analysis of seven zircon cores from the Concordia Granite yields a concordia age of 1173 ± 15 Ma suggesting that an age of ca. 1170 Ma most likely represents the true emplacement age of the Concordia Granite. The mean 207Pb/206Pb age of 1042 ± 9 Ma obtained on zircon from the main coarse-grained vein is interpreted as the crystallization age of the vein. 207Pb/235U monazite ages are highly variable in the veins and Concordia Granite host, ranging from ca. 1050 to 1000 Ma. This supports the petrographic and mineral chemistry evidence that the monazite U--Pb system was variably affected by a continuous or multi-pulse metasomatic/metamorphic event(s) occurring between 1050 and 1000 Ma. U--Pb analyses of deformed monazite crystals from a radioactive sinistral shear zone of the Kliphoog area yield a mean 207Pb/235U age of ca. 1006 ± 9 Ma, indicating that the late circulation of Th-LREE-rich fluids synchronous with strike-slip deformation occurred at ca. 1000 Ma. On a regional scale, the intrusion of the Kliphoog coarse-grained vein is contemporaneous with granulite-facies metamorphism as well as the A-type granitoid magmatism of the Spektakel Suite, mafic magmatism of the Koperberg Suite, and emplacement of the monazite vein-type deposit at Steenkampskraal. Therefore, a genetic relationship between the formation of monazite-rich Kliphoog veins and these metamorphic, magmatic, and metallogenic events is proposed.
•REE- and actinide-rich charnockite veins Kliphoog, Namaqualand, South Africa.•Vein formation results from intrusion of REE- and actinide-rich melts and fluids.•Alteration of zircon and monazite in the granitoid veins record/time metasomatic events.
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7.
Media Spectacle Kellner, Douglas
2003, 20030829, 2004-01-14, 2003-08-29, 20020101
eBook
During the mid-1990s, the O.J. Simpson murder trial dominated the media in the United States and were circulated throughout the world via global communications networks. The case became a spectacle ...of race, gender, class and violence, bringing in elements of domestic melodrama, crime drama and legal drama. According to this fascinating new book, the Simpson case was just one example of what the author calls 'media spectacle' - a form of media culture that puts contemporary dreams, nightmares, fantasies and values on display. Through the analysis of several such media spectacles - including Elvis, The X Files, Michael Jordan, and the Bill Clinton sex scandals - Doug Kellner draws out important insights into media, journalism, the public sphere and politics in an era of new technologies.
In this excellent follow up to his best selling Media Culture, Kellner's fascinating new volume delivers an informative read for students of sociology, culture and media.
•A continuum of Paleoproterozoic heritage, seen in Nd model ages, from N to S in the Bushmanland Domain (BD), with the Buffels River shear zone simply a regional discontinuity.•The southern BD (SBD) ...has a greater juvenile component than the northern BD (NBD), becoming more dominant post-1.10 Ga.•Orthogneisses derived from crustal magmas with subduction-influenced signatures with mixed Meso- to Paleoproterozoic model ages. The SBD Koperberg Suite derived from low degrees of melting of enriched SCLM, but at deeper levels than those of the NBD.•The paragneisses derived from largely reworked, mixed Meso- to Paleoproterozoic felsic to intermediate sources.•Paragneisses derived from largely reworked, mixed Meso- to Paleoproterozoic felsic to intermediate sources.•SBD Koperberg Suite derived from low degrees of melting of enriched SCLM, but at somewhat deeper levels than NBD Koperberg magmas.•D2 deformation constrained to ~ 1.11-1.09 Ga, with peak M3 metamorphism at ~ 1.05-1.02 Ga.
The timing of tectonomagmatic events and petrogenesis of ortho- and paragneisses within the high-grade southern Bushmanland Domain (SBD) of the Namaqua Metamorphic Province is, largely, poorly constrained. U-Pb age dating and whole rock lithogeochemistry of the rocks of the upper granulite facies Kliprand dome provide constraints with regards to the evolution of the SBD during the 1.2–1.0 Ga Namaquan Orogeny.
The SBD has a greater juvenile component, particularly added between ∼1.1 and 1.02 Ga, compared to the northern Bushmanland Domain (NBD). This is reflected in marginally younger TDM model ages (1.60–1.95 Ga) than for the NBD (∼1.9–2.4 Ga), and higher εNd(t) values for magmatic rocks, particularly for the late- to post-tectonic Spektakel Suite (SS), concentrated in the SBD. The ∼1.06 Ga Klein Lieslap Charnockite of the SS was derived from reworking of radiogenic Paleoproterozoic arc crust, but has a large juvenile depleted component compared to that of the ∼1.19 Ga Grootberg Gneiss of the syn-tectonic Little Namaqualand Suite.
SBD mafic magmas were derived from low degrees of partial melting of subduction-influenced enriched subcontinental lithospheric mantle. The pre-tectonic ∼1.17 Ga Oorkraal Suite shows limited crustal contamination of mantle-derived melts. The post-tectonic ∼1.05 Ga Koperberg Suite was derived from deeper mantle melting than that in the NBD, but shows less crustal contamination. The supracrustal Kamiesberg Group was derived from mixed, reworked Meso- to Paleoproterozoic crust that showed a more dominant depleted component compared to that in the NBD. Incongruent anatexis of the paragneisses gave rise to crosscutting garnetiferous quartzofeldspathic segregations, notably the strongly peraluminous ∼1.07 Ga Ibequas Leucogranite.
D2 deformation, at ∼1.11–1.09 Ga, resulted in penetrative foliation. D3 deformation, related to the development of a sub-vertical foliation in the limbs of F2 folds, is constrained to ∼1.07–1.06 Ga, between emplacement of the Ibequas Leucogranite and the Koperberg Suite. Peak granulite facies M3 metamorphism occurred at ∼1.05–1.02 Ga. These age constraints are similar to those of the NBD reflecting a synchronous tectonomagmatic and kinematic history. The SBD represents a deeper crustal level with a greater mantle influence than the NBD.
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GEOZS, IJS, IMTLJ, KILJ, KISLJ, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, UL, UM, UPCLJ, UPUK, ZRSKP
Was sich 2015 ereignete, war kein voraussetzungsloses, plötzliches Erscheinen und keine Krise der Migration, sondern eine Krise des europäischen Grenzregimes. Neben den eigensinnigen und ...widerständigen Bewegungen der Migration war diese Zeit gekennzeichnet von zivilem Engagement und von zahlreichen Kunst- und Kulturproduktionen mit, für und über Geflüchtete. Nanna Heidenreich fragt ausgehend vom ›langen Sommer der Migration‹ nach dem Verhältnis von Hype zu Möglichkeitsraum: Wann wird Kunst mit Migration zum Spektakel? Wie stehen ästhetische Schwellenerfahrungen zum Anspruch auf politische Transformation? Auf welche Weise sind Klimawandel und Migration miteinander verschaltet, von wessen Zukunft reden wir? Und welche Farbe hat das Meer?
This work presents current approaches and new avenues of enquiry into ancient sport and spectacle. It discusses historical perspectives, contest forms, contest-related texts, civic and social ...aspects, and use and meaning of the individual body. Greek and Roman topics are interwoven under each heading to simulate contest-like tensions and complementarities, juxtaposing, for example, violence in Greek athletics and in Roman gladiatorial events, Greek and Roman chariot events, architectural frameworks for contests and games in the two cultures, and contrasting views of religion, bodily regimens, and judicial classification related to both cultures. It examines the social contexts of games, namely the evolution of sport and spectacle diachronically and geographically across cultural and political boundaries, and how games are adapted to multiple contexts and multiple purposes, reinforcing, for example, social hierarchies, performing shared values, and playing out deep cultural tensions. The work also pays some attention to other directing forces in the ancient Mediterranean (e.g. Bronze Age Egypt and the Near East; Etruria; and early Christianity). The volume addresses important themes common to antiquity and modern society, such as issues of class, gender, health, and the popular culture of the modern Olympics, and gladiators in cinema. It presents contests and spectacles as venues of connection and as opportunities for the negotiation of status and the exchange of value, broadly for example how early panhellenic sanctuaries responded to economic stakeholders, and how groups and individuals in the later Roman empire forged social and political links through the circus events.
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