Dissertations / Theses on the topic 'Hf isotopes zircon'
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Pepper, Martin Bailey. "Magmatic History and Crustal Genesis of South America: Constraints from U-Pb Ages and Hf Isotopes of Detrital Zircons in Modern Rivers." Diss., The University of Arizona, 2014. http://hdl.handle.net/10150/347220.
Full textCouzinié, Simon. "Evolution of the continental crust and significance of the zircon record, a case study from the French Massif Central." Thesis, Lyon, 2017. http://www.theses.fr/2017LYSES035.
Full textThe formation of the continental crust is a major consequence of Earth differentiation. Understanding how the crust formed and evolved through time is paramount to locate the vast mineral deposits hosted therein and address its influence on the global climate, ultimately affecting the development of terrestrial life. Recent advances on the topic of continental crust evolution benefited from improvements of analytical techniques enabling in situ measurements of U-Pb- Hf-O isotope compositions in zircon, a widespread accessory mineral of continental igneous rocks. The time constrains derived from the U-Pb chronometer coupled with the petrogenetic information retrieved from Hf-O isotope signatures are currently used to unravel the diversity and succession of magmatic events affecting the continental crust at the regional and global scales. This study reconstructs the evolutionary path followed by the crust segment today exposed in the eastern part of the French Massif Central (FMC), a portion of the Variscan belt of Western Europe, with the aim to investigate the potential flaws of the zircon record of crust evolution. In this scope, the origin and geodynamic significance of the constituent FMC lithological units are tackled by combining conventional petrological observations with zircon U-Pb-Hf-O isotope data. The results obtained following this integrated approach are then confronted to the conclusions that would have been drawn solely from zircon isotopic signatures, taken out of their petrological context, as is commonly performed in studies investigating crust evolution. The oldest rocks of the FMC correspond to Ediacaran (590_550 Ma) meta-sediments deposited in back-arc basins along the northern Gondwana margin. Such basins were fed by a mixed detritus originating from the adjacent Cadomian magmatic arc and a distal Gondwana source, presumably the Sahara Metacraton. Partial melting of these meta-sediments at the Ediacaran/Cambrian boundary led to voluminous S-type granitic magmatism, pinpointing a first major crust reworking event in the FMC. The origin of anatexis likely stems from the transient thickening of the hot, back-arc crust caused by the flattening of the Cadomian subduction. Subordinate melting of the depleted backarc mantle at that time is also documented. During the Lower Paleozoic, rifting of the northern Gondwana provoked coeval crust and (limited) mantle melting. Mantle-derived igneous rocks show markedly diverse trace element and isotopic signatures, consistent with a very heterogeneous mantle source pervasively modi_ed by the Cadomian subduction. Finally, the Variscan collision resulted in crustal melting as evidenced by the emplacement of S-type granites and the formation of migmatite domes, the spatial distribution of which being partly controlled by the crustal architecture inherited from pre-orogenic events. Synchronous intrusion of mafic mantle-derived magmas and their differentiates testify for Variscan post-collisional new continental crust production in the FMC. Two major inconsistencies exist between these results and the zircon record. First, zircon Hf model ages would point to substantial Mesoproterozoic crust formation in the FMC whereas more than 60% of the crust is actually Neoproterozoic in age. Second, new additions to the continental crust volume during the Variscan orogeny are not recorded even though 5 to 10% of the exposed crust formed at that time. The origin of both discrepancies inherently lies in the mixed isotopic signature carried by many zircon grains. Such equivocal information can only be detected when additional petrological constrains on the zircon host rocks are available and provide guidance in interpreting the zircon record of crust evolution
Liu, Chaohui, and 刘超辉. "Paleoproterozoic basins in the Trans-North China Orogen: stratigraphic sequences, U-PB ages and HF isotopes of detritalzircons and tectonic implications." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B47163902.
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Earth Sciences
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Doctor of Philosophy
Reid, Mattie Morgan. "Forearc basin detrital zircon provenance of Mesozoic terrane accretion and translation, Talkeetna Mountains-Matanuska Valley, south-central Alaska." Thesis, University of Iowa, 2017. https://ir.uiowa.edu/etd/5611.
Full textGudelius, Dominik [Verfasser], and A. [Akademischer Betreuer] Zeh. "Petrogenetic Significance of Zircon in Mafic and Felsic Rocks of the Bushveld Complex: Melt Inclusions, Physicochemical Conditions and Hf Isotopes / Dominik Gudelius ; Betreuer: A. Zeh." Karlsruhe : KIT-Bibliothek, 2020. http://d-nb.info/1223027945/34.
Full textDemouy, Sophie. "La naissance des Andes au Crétacé supérieur : origine et construction du Batholite côtier sud-péruvien (région d'Arequipa)." Toulouse 3, 2012. http://thesesups.ups-tlse.fr/2201/.
Full textDuring the Late Cretaceous and Paleocene, intense magmatic arc activity resulted in the building of a continuous relief along the Peruvian margin. This arc growth coincided with the only known significant uplift along the coastal southern Peru. Our study has focused in the Arequipa area, on a batholith segment extending 80x60 km for a thickness bigger than 7 km. The structural study describes an object that is complex and consists of different plutonic units, that for some underwent extensive deformation syn to post emplacement. Major faults affect the batholith as a consequence of tectonic strains and exaggerate growth of the arc. The geochronological study indicates a discontinuous construction of the batholith, during the Jurassic (200-175 Ma) and the Late Cretaceous-Paleocene (90-60 Ma). Exploitation of the geochemistry and isotopic data (Hf, Sr, Nd) allows to identify an initiation stage of the arc during which fractional crystallization and mixing are predominant, and a thermal maturation stage during which magmas are homogenized in the deep crust, and evolve by fractional crystallization until the batholith level. This period leads to the construction of more than 70 % of the batholith and can thus be considered as a flare-up event. This event is characterized by juvenile signatures and also contributes significantly to the growth of the continental crust
Canile, Fernanda Maciel. "Geologia isotópica em zircões detríticos (U-Pb, Hf e O) e em rocha total (Sm-Nd e Pb-Pb) das rochas da Bacia do Paraná em Santa Catarina." Universidade de São Paulo, 2016. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-24022016-140417/.
Full textU-Pb, Hf and O isotope data were obtained from detrital zircons from late Paleozoic-early Mesozoic units from Paraná Basin, southeastern Brazil, in order to constain the provenance of the sediments, as well as to contribute to the understanding of the tectonic evolution of the basin. Whole rock Sm-Nd and Pb-Pb isotopic signatures were also taken in order to help the interpretation. The studied section, White Column in Santa Catarina state, includes rocks from 11 stratigraphic units (from base to top): Rio do Sul Formation, Rio Bonito Formation (Triunfo, Paraguaçu and Siderópolis members), Palermo Formation, Irati Formation, Serra Alta Formation, Teresina Formation, and Rio do Rasto Formation (Serrinha and Morro Pelado members) and Botucatu Formation. U-Pb ages were obtained on 1941 detrital zircons and range from 242 Ma to 3400 Ma. All sedimentary units show four main detrital age groups, Neoarchean (2700-2500 Ma), mid-Paleoproterozoic (2000-1800 Ma), Grenvillian (1100-900 Ma) and Brasiliano (850-490 Ma), reflecting the importance of the Precambrian basement bordering the east side of the basin, such as Dom Feliciano, Kaoko and Namaque-Natal Belts as source areas, including the local basement that was dated at 584 Ma. The Siderópolis Member shows an important change in the source of sediments with a Permian age-peak (266 to 290 Ma). This age-peak persists towards the top of the section until the Botucatu Formation. O and Hf isotopic signatures from the detrital zircons show that a portion of the mid-Paleoproterozoic grains is probably from rocks of the presently covered basement, which was exposed until the deposition of the Rio Bonito Formation. O and Hf isotopes also show that some Grenvillian aged zircons are from Argentinian rocks, which implies a long transport distance. Isotopic signatures of part of the Permian grains also link them to sources from Argentina and Chile, and part of these grains has more rounded shapes, suggesting that they reached the basin after long distance traveling on subaquatic environment and nor only through the air (ash falls) as it is commonly accepted. Other younger age peaks (Ordovician to Carboniferous) found from Palermo Formation upsection are also linked to Argentinian and Chilean sources, showing the importance of distant sources during the filling of the basin. The Sm-Nd and Pb-Pb data on whole rocks show that the sediments from the Paraná Basin present predominance of sources with crustal origin. Osotopic signatures are similar to granitoid rocks from Santa Catarina, Ribeira Belt, Brazilian Shield, Namaqua-Natal and Kaoko Belts, as well as the Arequipa-Antofalla terranes (Andes basement) and granitoids from North Patagonia. These data corroborate the observed detrital zircon patterns thar point to both proximal and distal source areas. \'T IND.DM\' model ages older than 1.4 Ga and more negative (-10 to -15) epsilon values were observed in the lower units (Rio do Sul Formation to Paraguaçu Member), while the upper units show \'\'épsilos\' IND.Nd(0)\' values ranging from -6 to -12 and \'T IND. DM\' model ages younger than 1.5 Ga, corroborating the addition of a younger source starting from the Siderópolis Member deposition upwards, as noted by detrital zircon data (Permian age-peak).
Guitreau, Martin. "Les isotopes de l'hafnium dans les TTG et leurs zircons : témoins de la croissance des premiers continents." Phd thesis, Ecole normale supérieure de lyon - ENS LYON, 2012. http://tel.archives-ouvertes.fr/tel-00713096.
Full textLuo, Yan. "U-Pb age and Hf isotopic study of detrital zircons from the Liaohe Group constraints on the evolution of the Jiao-Liao-Ji Belt, North China craton /." Click to view the E-thesis via HKUTO, 2005. http://sunzi.lib.hku.hk/hkuto/record/B36639242.
Full textXia, Xiaoping. "Spot U-Pband Hf isotope analyses of detrital zircons from the khondalites in the western block of the North China craton." Click to view the E-thesis via HKUTO, 2005. http://sunzi.lib.hku.hk/hkuto/record/B35773698.
Full textXia, Xiaoping, and 夏小平. "Spot U-Pband Hf isotope analyses of detrital zircons from the khondalites in the western block of the North China craton." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2005. http://hub.hku.hk/bib/B35773698.
Full textLuo, Yan, and 羅彥. "U-Pb age and Hf isotopic study of detrital zircons from the Liaohe Group: constraints on the evolution of theJiao-Liao-Ji Belt, North China craton." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2005. http://hub.hku.hk/bib/B36639242.
Full textVezinet, Adrien. "Différenciation et stabilisation de la croûte continentale archéenne, l'exemple de la marge Nord du craton du Kaapvaal en Afrique du Sud." Thesis, Lyon, 2016. http://www.theses.fr/2016LYSES054/document.
Full textThe PhD work presented in this manuscript focuses on the recognition and the manifestation of Archean crustal differentiation processes. The Archean eon which represents 1/3 of the geological record is featured by both lithologies unrecognized in younger eons and cryptic geodynamics. Most of investigations concentrate on the characterisation of aluminium-rich lithologies that allow an accurate determination of the pressure-temperature evolution underwent by crustal materials during crustal thickening geodynamics. However, aluminium-rich lithologies - mainly represented by metasediments - account for only 10% on average of Archean terranes whereas orthoderived gneisses - which also testify for crustal differentiation processes - form around 75% of these terranes. The following contribution depicts an Archean composite grey gneiss complex located at the northern edge of the Kaapvaal craton is South Africa. Results carried out during this PhD study have major consequences on Archean geodynamics. The zircon U-Pb/Lu-Hf isotope Investigation coupled with strong petro-metamorphic observations show that composite grey gneiss complexes may be built over a protracted time span, achieved through self-refinement of crustal materials, i.e. the crustal block evolved in a thermodynamically closed system. Grey gneiss compiexes are only moderately investigated even though information enclosed in these lithologies is complementary with those from aluminium-rich rocks. Therefore, deeper investigations of these geological objects must be a central scope in order to improve the knowledge of the Archean eon and appears necessary for the building of even more realistic geotectonic models
Linde, G. M., J. H. Trexler, P. H. Cashman, G. Gehrels, and W. R. Dickinson. "Three-Dimensional Evolution of the Early Paleozoic Western Laurentian Margin: New Insights From Detrital Zircon U-Pb Geochronology and Hf Isotope Geochemistry of the Harmony Formation of Nevada." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/626478.
Full textZeng, Wen. "The evolution of the metamorphic series in the NW Fujian Province, the NE Cathaysia Block, and the significance in the reconstruction of Precambrian Supercontinents." Thesis, Curtin University, 2010. http://hdl.handle.net/20.500.11937/1091.
Full textJustino, Dayvisson. "Geocronologia das sub-bacias triássicas Rincón Blanco e Cerro Pontudo, Argentina: combinação de metodologia U-Pb e Lu-Hf em zircão." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2016. http://hdl.handle.net/10183/158330.
Full textThe sub-basins Rincón Blanco and Cerro Puntudo are depocenter belonging to the northern part of the Cuyo Basin, exposed in an allochthonous terrane of Laurentia that was added to the Gondwana protomargin and now exposed in the Precordillera Argentina. The rift basin was filled predominantly of pyroclastic and continental clastic sediments, and is composed of many asymmetric grabens half-linked by accommodation zones. U-Pb and Lu-Hf zircon isotope analyses were carried out in the basement units and volcanoclastic rocks and tuffs of both Triassic sub-basins. Basement rocks were dated at 269.9±2.9 Ma with Hf model ages 1.34 to 1.60 Ga. The volcanoclastic rocks contain zircons crystallized from 238 Ma to 1433 Ma with main peak at Permian-Triassic and Stenian (1.0 to 1.2 Ga). The Triassic rhyolite and tuffs formed between 246 and 230 Ma and have Hf model ages ranging from 1.02 to 1.50 Ga. Indeed, the volcanoclastic rocks present dominant Mesoproterozoic ages, mostly correlated to the Grenvillian. Some zircon grains show Hf Paleoproterozoic model ages which are interpreted to be part of Gondwana cratonic areas. The presence of dominant Mesoproteorzoic favored the hypotheses of a Grevillian basement for the related acid magmatism of the Cuyo Basin and allocthonous Cuyan Terrane.
Yeshanew, Fitsum Girum. "Crustal evolution of the Arabian–Nubian Shield : Insights from zircon geochronology and Nd–Hf–O isotopes." Doctoral thesis, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-145479.
Full textAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 3: Manuscript. Paper 4: Manuscript.
Jeon, Heejin. "U-Pb, Lu-Hf and O isotopes in zircon from late palaeozoic granites across orogens, Southeastern Australia." Phd thesis, 2012. http://hdl.handle.net/1885/149621.
Full textReid, B. A. "Structural, geochronological and tectonic evolution of the central Eastern Ghats Province, India: Araku-Anantagiri-Visakhapatnam." Thesis, 2010. http://hdl.handle.net/2440/102762.
Full textThe central Eastern Ghats Province is part of a series of terranes that collectively form the Eastern Ghats in India. The Eastern Ghats is a Mesoproterozoic to early Neoproterozoic orogen associated with the formation of the supercontinent Rodinia, c. 1.1 to 0.95 Ga. The central Eastern Ghats Province consists of metaquartzites and metapelites (khondalites) that are intruded by granitoids. The location of proto-India within Rodinia is disputed because of recently presented palaeomagnetic data. This has generated confusion about whether the protoliths to the Eastern Ghats Province metasedimentary rocks were deposited adjacent to proto-India or as an exotic terrane later accreted to India. U-Pb geochronology, in conjunction with Hf isotopes of zircons, constrain the maximum depositional age, determine provenance and identify the location of deposition. A maximum depositional age of 1.14 Ga on the protoliths to the khondalites has been determined from U-Pb zircon geochronology. The short period of time between deposition and the orogenesis related thermal event indicates that the sediments were deposited adjacent to the Bastar Craton. Provenance work identifies a number of sources within India and east Antarctica lending support to the theory that these continents were contiguous prior to the Eastern Ghats Orogeny. Structural transects and mapping reveals that shortening associated with the collision of east Antarctica and proto-India occurred along a NE-SW trending axis.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Priyatkina, Nadezhda. "The Proterozoic history of the northern and western Siberian cratonic margins based on results of U-Pb-Hf detrital zircon analysis." Thesis, 2017. http://hdl.handle.net/1959.13/1383756.
Full textAlong the western and northern margins of the Siberian Craton the Proterozoic sedimentary formations form pre-orogenic and post-orogenic sedimentary cycles, separated by a major unconformity. In various uplifts of Meso-to Neoproterozoic sedimentary rocks of Siberian cratonic margin, such as the Taimyr, the Yenisey Ridge and the Prisayan, detrital zircon signatures below the unconformity are compared with those of immature post-accretionary sedimentary rocks occurring above the unconformity. The data are further used to characterize the age of Early Precambrian basement and Neoproterozoic crust along the northern and western Siberian cratonic margins and to assist with identifying the tectonic setting of Neoproterozoic magmatic belts, their cratonic affinity and the overall geological evolution of these margins. It has been confirmed that Siberian cratonic basement is heterogenous in its age. Along the southwestern cratonic margin (Prisayan Uplift) the basins accumulated predominantly 3.4-2.7 Ga and 1.9-1.85 Ga detritus; along the western cratonic margin (Turukhansk Uplift, northern Yenisey Ridge), the basins accumulated predominantly 2.6–2.5 Ga and 1.9–1.85 Ga erosional products, while the main sources for the fill of intracratonic basin to the northeast near the Anabar Shield (East Anabar basin) were 2.9–2.7 Ga and 2.1–1.95 Ga old igneous rocks. The studied pre-orogenic rocks were mostly deposited during the Meso – to Early Neproterozoic rift-related or passive margin settings. Along with magmatic components of the Neoproterozoic crustal fringe, these rocks underwent major craton-wide recycling to produce late Ediacaran post-orogenic siliciclastic successions. Results of Hf in zircon study allow to identification of four distinct magmatic systems belt, associated with development of continental arcs at ca. 970-800 Ma and 720-600 Ma, and an oceanic arc at ca. 800-720 Ma in the Taimyr orogenic belt, and development of a long term continental arc during 950-600 Ma in the Yenisey Ridge and the north-western East Sayan. In addition to isotopic data, a geological evidence is discussed to support that Neoproterozoic crustal growth occurred near the northern and western Siberian margins and resulted in forming siginifcant portion of Arctic crust.
Henderson, B. J. "The tectonic evolution of the Ongole Domain, India: a metamorphic and geochronological approach." Thesis, 2011. http://hdl.handle.net/2440/96173.
Full textThe Ongole Domain, situated in the southern Eastern Ghats Belt, exposes an assemblage of granulite facies metasedimentary and metaigneous rocks that preserve fundamental evidence for the Paleoproterozoic-Mesoproterozoic reconstruction of the supercontinent Nuna. LA-ICP-MS detrital zircon data from metasedimentary rocks constrain the timing of deposition for the sedimentary precursors, to between ca. 1850-1750 Ma. Lu-Hf isotopic data from detrital zircons provide a wide range of εHf values between -18 and +10, and TDM of ca. 3.2- 2.6 Ga. The Mesoarchean to Paleoproterozoic detrital components display geochemical similarities with the Napier Complex, the North Australian Craton and to a lesser extent, the North China Craton. U-Pb zircon and monazite geochronology have identified three episodes of metamorphism in the Ongole Domain; at ca. 1750, 1640 and 1590 Ma. Peak P-T estimates of 900 - 910°C and 9 - 9.2 kbar are calculated for metamorphism associated with collisional orogenesis, between ca. 1640-1590 Ma. Ti-in-zircon thermometry independently constrains the UHT conditions, yielding estimates of 935 ± 55°C. U-Pb geochronology and trace element analysis of zircon grains from metaigneous rocks confirm syn-tectonic magmatism occurred in the Ongole Domain between ca. 1640-1570 Ma. The results provide support for paleogeographic reconstructions that link the southern Eastern Ghats Belt and East Antarctica during the late Paleoproterozoic
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Al-Kiyumi, M. "Constraining the age and provenance of the basal quartzites of the Centralian Superbasin." Thesis, 2018. http://hdl.handle.net/2440/130321.
Full textThe Heavitree Formation of the Amadeus Basin, central Australia, is thought to correlate with a number of similar formations in the Officer, Ngalia, Georgina and Murraba Basins that formed the Centralian Superbasin. The Jasper Gorge Formation of the Victoria Basin and Jamison Sandstone of the Beetaloo Sub-basin are also thought to be corollaries. These formations are all constrained to being younger than ca. 1.0 Ga by U-Pb detrital zircon studies. However, in all cases, this is suspected to considerably pre-date the timing of deposition. Here, we present new U-Pb and Hf data from seven samples of the Amadeus Basin Heavitree Formation to a) better constrain the age of the Heavitree Formation, b) investigate the spatial variation in provenance of the Heavitree Formation, and, c) compare it with other ‘Supersequence 1’ quartzites from the wider Centralian Superbasin.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2018
Robinson, Frank Alexander. "Geochronological and geochemical constraints on the lithospheric evolution of the Arabian shield, Saudi Arabia: understanding plutonic rock petrogenesis in an accretionary orogen." Thesis, 2014. http://hdl.handle.net/2440/84674.
Full textThesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2014
Hsu, Chun-Chieh, and 許鈞傑. "Detrital Zircon U-Pb and Hf Isotopic Study in Northwestern Sumatra, Indonesia." Thesis, 2016. http://ndltd.ncl.edu.tw/handle/25561429169923275462.
Full text國立臺灣大學
地質科學研究所
104
In NW Sumatra, Tertiary sedimentary basins that occur in forearc and backarc settings with respect to the present-day subduction system were deposited in three major terranes, namely, the Woyla Nappe, the East Sumatra block, and the West Sumatra block. NW Sumatra represents the product of complex accretion/collision/subduction histories among these three terranes, which have originated from the eastern margin of Gondwanaland. To better understand the complex histories, we present a detrital zircon study in NW Sumatra that, together with our unpublished work on major magmatic rocks in the area, allow us to reach the following conclusions: (1) Detrital zircons from 14 samples (river sand or sandstone) in the forearc basin reveal seven age peaks at ~1050 Ma (n=74), ~550 Ma (n=65), ~214 Ma (n=138), ~131 Ma (n=14), ~100 Ma (n=65), ~52 Ma (n=238) and 17-0 Ma (n=303), respectively; (2) Detrital zircons from nine samples in the backarc basin show similar age populations; (3) The Late Triassic zircons, with εHf(T) values of -18 to 0, are sourced mainly from the Indosinian granitoids that are widespread in the East Sumatra block; (4) The less abundant Early Cretaceous zircons, with εHf(T) values of -5 to 0, are most likely from the West Sumatra block; (5) The Late Cretaceous zircons, with εHf(T) values of +11 to +16, are from the Woyla Nappe due probably to the Woyla accretion; (6) The Eocene and younger zircons, with εHf(T) values of +6 to +17, are from the initial stage and modern arc magmatic rocks related to the Indian Ocean plate subduction.
Shao, Wen-Yu, and 邵文佑. "Zircon U-Pb and Hf isotope constraints on the petrogenesis of igneous rocks in eastern Taiwan." Thesis, 2015. http://ndltd.ncl.edu.tw/handle/54490476633081385630.
Full text國立臺灣大學
地質科學研究所
103
This thesis reports new zircon U-Pb and Lu-Hf isotopic data to better understand the petrogenesis of igneous rocks from eastern Taiwan. These include (1) volcanics from the Coastal Range, Lutao and Lanyu, (2) ophiolitic rocks from the Lichi melange, and (3) glaucophane-bearing rocks from Juisui area, the Yuli belt. Magmatic zircons yielded mean 206Pb/238U ages of 9.2 ~ 4.2 Ma for Coastal Range volcanics, ~2.6 Ma for Lanyu volcanics, ~1.3 Ma for Lutao volcanics, 17.5 ~ 14.1 Ma for east Taiwan ophiolitic rocks, and 16.0 ~ 15.4 Ma for the protolith of Juisui blueschists, respectively. We speculate that the subduction of South China Sea plate beneath the Philippine Sea plate has been initialized since ~20 Ma, and the mean inherited zircon 206Pb/238U ages of ~14.2 Ma from the Chimei igneous complex might be the earliest product of north Luzon arc magmatism. In general, magmatism in the Coastal Range had been terminated soon after the Penglai orogeny (6 ~ 5 Ma) and the final magmatism occurred at ~4.2 Ma. However, the arc magmatism of Lanyu and Lutao still spanned from Pliocene to Pliestocene. Besides, abundant inherited zircons have been obtained from the Chimei igneous complex, Yuemei volcanics, Chimei volcanics, and Lanyu volcanics, providing significant evidence for the existence of Cathaysia-affinity continental fragments rifted by the opening of the South China Sea were underneath the Luzon volcanic arc. The presence of abundant inherited zircons in volcanics suggests the magmas ascent though the old continental crust, feeding the Miocene arc, picked up the ancient zircons through assimilation or partial melting. Based on the increasing zircon uranium concentrations and the decreasing zircon εHf(T) values, we speculate that the continent-ward approach of the Manila trench allowing much more enriched continental material to involve into the mantle wedge. The magmatism of the east Taiwan ophiolite occurred during mid-Miocene, including gabbros of 17.5 ~ 17.4 Ma, diorite of 14.3 Ma and plagiogranites of 14.3 ~ 14.1 Ma. Based on the abundant inherited zircons from the ~17.5 Ma gabbro, we suggest a process of crustal contamination in ETO’s magmas during ~17.5 Ma. Moreover, the zircon Hf isotopic data indicated that the magmas were more depleted through time. In this study, we consider that the ETO originated from the highly depleted forearc magmas due to the subduction initiation of the South China Sea plate and incorporated into the Lichi melange as allochthonous blocks during the late Miocene-early Pliocene Penglai orogeny. The magmatic ages of protolith of Juisui blueschists can be well-constrained at 16.0 ~ 15.4 Ma by the zircon U-Pb ages, instead of exotic/tectonic blocks that were thought to be mid-Cretaceous or older ocean-floor fragments. Thus, we speculate that the Yuli metamorphic belt should have taken place after mid-Miocene. Based on the zircon εHf(T) variations (~32 ε-units) and whole-rock geochemistry (high MnO content), we suggest that the protolith of Juisui blueschists was product which mixed from depleted magmas (mantle-derived), enriched continental material, and Mn-rich deep-sea sediments. The protolith had undergone a high-pressure blueschist facies metamorphism and eventually rapidly exhumed and accreted to the eastern slope of the Central Range during the late Cenozoic. Briefly, the consensus of “paired metamorphic belts” of Taiwan should be thus falsified.
Ickert, Ryan Ben. "U-Pb, Lu-Hf, and O isotope systematics of zircon from southeastern Australian Siluro-Devonian granites." Phd thesis, 2010. http://hdl.handle.net/1885/147724.
Full textIshwar, Kumar C. "Mesoproterozoic Suturing Of Archean Crustal Blocks In Western Peninsular India : New Insights On India-Madagascar Correlations." Thesis, 2015. http://hdl.handle.net/2005/2651.
Full textHoward, K. E. "Provenance of Palaeoproterozoic metasedimentary rocks in the eastern Gawler Craton, Southern Australia: Implications for reconstruction models of Proterozoic Australia." Thesis, 2006. http://hdl.handle.net/2440/123593.
Full textDetrital zircon ages obtained from the Corny Point Paragneiss and the Massena Bay Gneiss in the southeastern Gawler Craton, Australia, constrain their deposition to the interval ca. <1880 Ma. The presence of 2020 Ma, 2450 Ma and 2520 Ma detrital zircons within the Corny Point Paragneiss constrains the source region for the sedimentary protoliths to three possible domains within Australia; the Gawler Craton, the Glenburgh Orogen in the Western Australian Proterozoic, and the North Australian Craton, all of which contain rock systems with similar ages. Whole rock εNd (1850Ma) values from the Corny Point Paragneiss range from -1 to -5. These values potentially preclude the Late Archaean to mid Proterozoic crust of the Gawler Craton as a sole or major source region due to its highly evolved average εNd (1850Ma) of around -10. Preclusion of the Gawler Craton as a source is apparently confirmed by Hf isotopic compositions of 2020 Ma detrital zircons from the Corny Point Paragneiss, which have εHf (2020Ma) ranging between +3 to +7. This compares with εHf (2020Ma) of -1 to -4 for zircons from the 2020 Ma Miltalie Gneiss in the Gawler Craton. Available Nd isotopic data suggests that the Glenburgh Orogen is too crustally evolved to have provided the majority of sediment into the Corny Point Paragneiss protolith. The 2020 Ma detrital Hf isotopic compositions of the Corny Point Paragneiss are similar to the 2020 Ma Wildman Siltstone (εHf (2020Ma) +2 to +7) in the Pine Creek Orogen in the North Australian Craton. Two possible scenarios can be extrapolated from the detrital zircon and Nd isotopic data; (1) the Corny Point Paragneiss sediment was derived from a source region within the North Australian Craton and could share source regions with the Wildman Siltstone, or (2) the sediments were derived from a Gawler Craton source region that included a dominant juvenile component of the 2020 Ma Miltalie Gneiss in the adjacent Gawler Craton which has since been eroded. In the first scenario, the absence of connection to the Gawler Craton allows for the Betts and Giles (2006) plate reconstruction model, which proposes that the Corny Point Paragneiss formed part of the North Australia Craton, and was sutured to the Proto Gawler Craton at 1730-1700 Ma. The second scenario highlights a significant limitation in evaluating the significance of provenance data, particularly when considering old potential source terrains that have undergone significant levels of denudation. The proximity of the Corny Point Paragneiss to the rifted southern and eastern margins of the Australian Proterozoic means a thorough evaluation of the palaeogeographic significance of the Corny Point Paragneiss detrital signature requires corresponding datasets from regions such as Antarctica which were formerly contiguous with the Gawler Craton.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2006
Chiu, Han-Yi, and 邱瀚毅. "The Neotethyan subduction and Zagros orogeny:constraints from zircon U-Pb age and Hf isotopic study ofmagmatic rocks from Iran." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/76570780192304152961.
Full text國立臺灣大學
地質科學研究所
101
This study reports the first combined LA-ICPMS analyses of zircon U-Pb and Hf isotope compositions for magmatic rocks from several major domains of Iran, including the Urumieh-Dokhtar magmatic arc (UDMA), Sanandaj-Sirjan structural zone (SSZ), Alborz Range, Central Iran and Sistan suture zone. These results, together with the literature data and some unpublished ages of our team, better delineate the magmatic evolution related to the Neotethyan subduction and subsequent Zagros orogeny that resulted from the Arabia-Eurasia collision. Moreover, this study also identifies two major magmatic events that formed during the late Neoproterozoic to Cambrian and the Late Triassic before the occurrence of broad magmatic activities which are related to the Neotethyan subduction. The first magmatic event represents a depleted mantle-derived magmatic feature and it has associated with the magmatism that produced the peri-Gondwanan terranes and Arabian-Nubian Shield. The second magmatic event is attributed to the Paleotethys evolution and shows an obvious magmatic signature of crustal contamination. The Neotethyan subduction-related magmatism was active during the Jurassic time, as evidenced by the presence of widespread I-type granitoids from the Middle to Late Jurassic (176-144 Ma) in the SSZ. These intrusive rocks, also exposed in the central part of the UDMA and the northern Lut block, show a heterogeneous isotopic affinity with variable zircon εHf(T) values between +12 and -5. After a protracted magmatic quiescence in the Early Cretaceous, the igneous activity renewed inland in the UDMA from which the Late Cretaceous granitoids (81-72 Ma) are found in the southeastern segment of the UDMA. These rocks from the Jiroft and Bazman areas have very different zircon εHf(T) values clustering from +15 to +11 and from +5 to -9, respectively, implying that the Bazman magmas were significantly mixed with the old crustal components. Then, the UDMA volcanism was most active and widespread during the Eocene and Oligocene (55-25 Ma), much longer lasting than the previously thought as just an Eocene pulse. Such a prolonged igneous “flare-up” event in the UDMA can be correlated to Armenia where the coeval calc-alkaline rocks are common. Similar ages are also obtained from the magmatic rocks in the northwestern SSZ and west Alborz. This magmatism, with mostly positive zircon εHf(T) values between +17 and -1, can further signify the formation of extensive juvenile crust in the regions owing to the Neotethyan subduction. The magmas with a primitive signature were also exposed in the southern Sistan suture zone and the Makran region during the Oligocene to Quaternary (32-1 Ma). By contrast, the ancient continental crust material was observed from the Central Iran, in Saghand area by the Eocene granitoids that yielded less radiogenic zircon Hf isotopes of εHf(T) values ranging from +6 to -7. The UDMA magmatism ceased progressively from the northwest to the southeast, with the magmatic activities ending in the Early Miocene (ca. 22 Ma) in Meghri, in the Middle Miocene (ca. 16 Ma) in Kashan and in the Late Miocene (ca. 10-6 Ma) in Anar. The southeastward magmatic cessation is consistent with the notion of the oblique and diachronous continental collision between Arabia and Eurasia. The post-collisional volcanism started at ca. 11 Ma in Saray, east off the Urumieh Lake, which, along with the later eruptions in Sahand (6.5-4.2 Ma) and Sabalan (≤0.4 Ma) volcanoes, forms a compositionally unique component of the vast volcanic field covering much of the Lesser Caucasus, NW Iran and eastern Anatolia regions.
Hiess, Joseph. "Early crustal petrogenesis : integrated in situ U-Pb, O, Hf and Ti isotopic systematics of zircon from Archaean rocks, West Greenland." Phd thesis, 2008. http://hdl.handle.net/1885/150388.
Full textChen, Bei. "Growth of the Preserved Continental Crust: Integrated U-Pb, O, and Hf isotopic systematics of detrital zircons from Australia and Antarctica." Phd thesis, 2022. http://hdl.handle.net/1885/267270.
Full textCastillo, Gonzalez Paula Alejandra. "Evolution of the patagonian-west antarctica margin of gondwana in the palaeozoic–early mesozoic: new models constrained by zircon u-pb ages, and o and hf isotopic compositions." Phd thesis, 2016. http://hdl.handle.net/1885/130073.
Full textKlama, Kai Olaf [Verfasser]. "U-Pb-Geochronologie, Hf-Isotopie und Spurenelementgeochemie detritischer Zirkone aus rezenten Sedimenten des Orange- und Vaal-River-Flusssystems in Südafrika / von Kai Olaf Klama." 2008. http://d-nb.info/994793383/34.
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