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| 1 | Prograde and retrograde growth of monazite in migmatites:An example from the Nagercoil Block,southern India显示文摘Data from a migmatised metapelite raft enclosed within charnockite provide quantitative constraints on the pressure-temperature-time[P-T-t) evolution of the Nagercoil Block at the southernmost tip of peninsular India.An inferred peak metamorphic assemblage of garnet,K-feldspar.sillimanite,plagioclase,magnetite,ilmenite,spinel and melt is consistent with peak metamorphic pressures of 6-8 kbar and temperatures in excess of 900℃.Subsequent growth of cordierite and biotite record high-temperature retrograde decompression to around 5 kbar and 800 C.SHRIMP U-Pb dating of magmatic zircon cores suggests that the sedimentary protoliths were in part derived from felsic igneous rocks with Palaeoproterozoic crystallisation ages.New growth of metamorphic zircon on the rims of detrital grains constrains the onset of melt crystallisation,and the minimum age of the metamorphic peak,to around560 Ma.The data suggest two stages of monazite growth.The first generation of REE-enriched monazite grew during partial melting along the prograde path at around 570 Ma via the incongruent breakdown of apatite.Relatively REE-depleted rims,which have a pronounced negative europium anomaly,grew during melt crystallisation along the retrograde path at around 535 Ma.Our data show the rocks remained at suprasolidus temperatures for at least 35 million years and probably much longer,supporting a long-lived high-grade metamorphic history.The metamorphic conditions,timing and duration of the implied clockwise P-T-t path are similar to that previously established for other regions in peninsular India during the Ediacaran to Cambrian assembly of that part of the Gondwanan supercontinent. | Tim E.Johnson Chris Clark Richard J.M.Taylor M.Santosh Alan S.Collins | 2015 | Geoscience Frontiers2015，6，3： | 8 |
| 2 | Mineralogical Evidence for Regional Metamorphism Overprinted by Contact Metamorphism显示文摘The Soursat metamorphic complex(SMC) in northwestern Iran is part of the Sanandaj-Sirjan metamorphic belt.The complex is composed of different metamorphic and plutonic rocks,but is dominated by metapelites composed of garnet,staurolite,kyanite,fibrolite,cordierite,and andalusite.Porphyroblasts in schists have the same fabric,and three stages of schistosity are present.The internal schistosity(Sn) inclusion trails are also offset by conjugate sets of extensional schistosity(Sn+1) and a second(Sn+2) that crenulates(Sn+1).Polyphase metamorphisms are present in the complex.Garnet,staurolite,kyanite,and fibrolite assemblage preserves conditions during the M1 metamorphic event.This assemblage yields a P-t estimate of 645±11°C and 6.5±0.5 kbar.Other samples of the central part of SMC contain cordierite and andalusite(M2) overgrowth that yields a P-t estimate of 532±33°C and 2.1±1.1 kbar. | Mahboobeh JAMSHIDI BADR Fariborz MASOUDI Alan S.COLLINS Ali SORBI | 2012 | Acta Geologica Sinica(English Edition)2012，86，1： | 3 |
| 3 | Tracking the Cretaceous transcontinental Ceduna River through Australia:The hafnium isotope record of detrital zircons from offshore southern Australia显示文摘The middle-upper Cretaceous Ceduna River system traversed continental Australia from the NE coast to the centre of the southern coast.At its mouth,it formed a vast delta system that is similar in scale to the Niger delta of West Africa.The delta system is composed of two main lobes that represent different phases of delta construction.A recent hypothesis has challenged the traditional idea that both lobes of the delta were derived from a transcontinental river system by suggesting that the upper lobe(Santonian- Maastrichtian) is instead derived from a restricted catchment within southern Australia.Hf isotopic data presented here fingerprint the original source of the upper delta lobe zircons to NE Australia,with data comparing well with similar U-Pb and Lu-Hf isotopic data from the Lachlan Orogen,the New England Orogen,the eastern Musgraves Province and the northern Flinders Ranges.These data do not preclude a model where the lobe is derived from recycled Eromanga Basin sediments during a phase of late Cretaceous inland Australian uplift,but when coupled with reconnaissance low-temperature thermochronometry from the region of the Ceduna River course indicating widespread Triassic-Jurassic exhumation,and comparisons with detrital zircon data from the Winton Formation upstream of any proposed uplift,we suggest that both lobes of the Ceduna Delta are likely to be derived from a transcontinental Ceduna River. | Jarred Lloyd Alan S.Collins Justin L.Payne Stijn Glorie Simon Holford Anthony J.Reid | 2016 | Geoscience Frontiers2016，7，2： | 2 |
| 4 | Late Neoproterozoic adakitic magmatism of the eastern Arabian Nubian Shield显示文摘Late Neoproterozoic adakitic magmatism within the Eastern Arabian Nubian Shield has been dated at633.2±9.0 Ma(2σ).These magnas intrude the forearc Ad Dawadimi Basin,which is composed of metapelitic schists and greywacke along with ophiolitic melanges of boninitic affinity which underwent inversion and deformation by^620 Ma.This adakitic magmatism,while intruding parts of the Ad Dawadimi Basin,predates this deformation,but is possibly coincident with basin closure.As adakitic magmatism requires melting of an amphibolite or eclogitic source,empirical and experimental constraints require anomalously hot supra-subduction zone mantle.Considering that this magmatism immediately predates basin inversion,these magmas possibly pinpoint the timing of the slab breaking,marking the terminal stages of arc magmatism,terrane accretion and the influx of hot oceanic asthenospheric mantle.This influx of hot asthenospheric mantle may also be responsible for postcolltsional A-type magmatism. | Grant M.Cox John Foden Alan S.Collins | 2019 | Geoscience Frontiers2019，10，6： | 2 |
| 5 | Late syn-to post-collisional magmatism in Madagascar:The genesis of the Ambalavao and Maevarano Suites显示文摘The East African Orogen involves a collage of Proterozoic microcontinents and arc terranes that became wedged between older cratonic blocks during the assembly of Gondwana.The Ediacaran-Cambrian Ambalavao and Maevarano Suites in Madagascar were emplaced during the waning orogenic stages and consist of weakly deformed to undeformed plutonic rocks and dykes of mainly porphyritic granite but also gabbro,diorite and charnockite.U-Pb geochronological data date emplacement of the Ambalavao Suite to between ca.580 Ma and 540 Ma and the Maevarano Suite to between ca.537 Ma and522 Ma.Major and trace element concentrations are consistent with emplacement in a syn-to postcollisional tectonic setting as A-type(anorogenic) suites.Oxygen(δ^(18)O of 5.27‰-7.45‰) and hafnium(ε(Hf)(t) of-27.8 to-12.3) isotopic data from plutons in the Itremo and Antananarivo Domains are consistent with incorporation of an ancient crustal source.More primitive δ^(18)O(5.27‰-5.32‰) andε(Hf)(t)(+0.0 to+0.2) isotopic values recorded in samples collected from the Ikalamavony Domain demonstrate the isotopic variation of basement sources present in the Malagasy crust.The Hf isotopic composition of Malagasy zircon are unlike more juvenile Ediacaran-Cambrian zircon sou rces elsewhere in the East African Orogen and,as such,Madagascar represents a distinct and identifiable detrital zircon source region in Phanerozoic sedimentary provenance studies.Taken together,these data indicate that high-T crustal anatexis,crustal assimilation and interaction of crustal material with mantle-derived melts were the processes operating during magma emplacement.This magmatism was coeval with polyphase deformation throughout Madagascar during the amalgamation of Gondwana and magmatism is interpreted to reflect lithospheric delamination of an extensive orogenic plateau. | Donnelly B.Archibald Alan S.Collins John D.Foden Justin L.Payne Peter Holden Théodore Razakamanana | 2019 | Geoscience Frontiers2019，10，6： | 2 |
| 6 | BMP Signaling in the Human Fetal Ovary is Developmentally Regulated and Promotes Primordial Germ Cell Apoptosis显示文摘 | Andrew J.Childs Hazel L.Kinnell Craig S.Collins KirstenHogg Rosemary A.L.Bayne Samira J.Green Alan S.McNeilly Richard A.Anderson | 2010 | STEM CELLS2010，，8： | 1 |
| 7 | Nature:人类基因组计划 回顾大生物学的25年显示文摘25年前,人类基因组计划启动了,时至今日,它所提供的经验仍旧指引着由它开启的、以团队协作为基础的科学研究。 | Eric D.Green James D.Watson Francis S.Collins | 2015 | 中国科技奖励2015，0，12： | 1 |
| 8 | An apatite U-Pb thermal history map for the northern Gawler Craton,South Australia显示文摘Apatite U-Pb thermochronology was applied to granitoid basement samples across the northern Gawler Craton to unravel the Proterozoic, post-orogenic, cooling history and to examine the role of major fault zones during cooling. Our observations indicate that cooling following the ~2500 Ma Sleaford Orogeny and ~1700 Ma Kimban Orogeny is restricted to the Christie and Wilgena Domains of the central northern Gawler Craton. The northern Gawler Craton mainly records post-Hiltaba Event(~1590 Ma) U-Pb cooling ages. Cooling following the ~1560 Ma Kararan Orogeny is preserved within the Coober Pedy Ridge,Nawa Domain and along major shear zones within the south-western Fowler Domain. The Nawa Domain samples preserve U-Pb cooling ages that are >150 Ma younger than the samples within the Coober Pedy Ridge and Fowler Domain, indicating that later(~1300 Ma) fault movement within the Nawa Domain facilitated cooling of these samples, caused by arc collision in the Madura Province of eastern Western Australia. When compared to^(40)Ar/^(39) Ar from muscovite, biotite and hornblende, our new apatite U-Pb ages correlate well, particularly in regions of higher data density. Our data also preserve a progressive younging of U-Pb ages from the nucleus of the craton to the periphery with a stark contrast in U-Pb ages across major structures such as the Karari Shear Zone and the Southern Overthrust, which indicates the timing of reactivation of these major crustal structures. Although this interpolation was based solely on thermochronological data and did not take into account structural or other geological data, these maps are consistent with the structural architecture of the Gawler Craton and reveal the thermal footprint of known tectonic and magmatic events in the Gawler Craton. | James W.Hall Stijn Glorie Anthony J.Reid Samuel C.Boone Alan S.Collins ANDrew Gleadow | 2018 | Geoscience Frontiers2018，9，5： | 1 |
| 9 | On the loss of saltmarshes in south‐east England and the relationship with Nereis diversicolor显示文摘 | R. K. A.MORRIS I. S.REACH M. J.DUFFY T. S.COLLINS R. N.LEAFE | 2004 | Journal of Applied Ecology2004，，4： | 1 |
| 10 | Accounting for Growth:Comparing China and India显示文摘 | Bosworth B S.Collins | | 0，，01： | 1 |
| 11 | Heightened central affective response to visceral sensations of pain and discomfort in IBS显示文摘 | G. B. C.Hall M. V.Kamath S.Collins S.Ganguli R.Spaziani K. L.Miranda A.Bayati J.Bienenstock | 2010 | Neurogastroenterology & Motility2010，，： | 1 |
| 12 | 人类基因组计划:大规模生物学的经验显示文摘21世纪是生命科学的世纪 ,人类基因组计划的完成必将促进医疗水平的提高 ;如果基础研究能继续这样被支持 ,相信人类很快能揭开心脏病、肿瘤、糖尿病、精神分裂症等疾病的奥秘——— | Francis S.Collins Michael Morgan Aristides Patrinos 胡鸣 | 2003 | 世界科学2003，，6： | 1 |
| 13 | 人类基因组计划对医学的影响显示文摘 | Francis S.Collins 欧阳晶 等 | 2001 | 美国医学会杂志(中文版)2001，20，6： | 1 |
| 14 | 成年囊性纤维化气管软化发病率和严重度的动态电影CT评价显示文摘目的应用动态电影多层CT,确定囊性纤维化(CF)成年病人气管软化的发生率和严重度,并将影像表现与肺功能测试(PFT)结果、肺实质病变严重程度相对照。方法本研究经伦理委员会批准并符合医疗健康保险要求,40例CF病人[男22例,女18例;年龄18~54岁。平均(22±8)岁];前瞻性行PFT,标准薄层CT和两次动态电影多层CT扫描。 | S.McDermott S.C.Barry E.E.Judge S.Collins P.A.Jong H.A.W.M.Tiddens 高莉 | 2009 | 国际医学放射学杂志2009，32，5： | 0 |
| 15 | Neoproterozoic tectonic geography of the south-east Congo Craton in Zambia as deduced from the age and composition of detrital zircons显示文摘The Southern Irumide Belt(SIB)is an orogenic belt consisting of a number of lithologically varied Mesoproterozoic and Neoproterozoic terranes that were thrust upon each other.The belt lies along the southwest margin of the Archaean to Proterozoic Congo Craton,and bears a Neoproterozoic tectonothermal overprint relating to the Neoproterozoic-Cambrian collision between the Congo and Kalahari cratons.It preserves a record of about 500 million years of plate interaction along this part of the Congo margin.Detrital zircon samples from the SIB were analysed for U-Pb and Lu-Hf isotopes,as well as trace element compositions.These data are used to constrain sediment-source relationships between SIB terranes and other Gondwanan terranes such as the local Congo Craton and Irumide belt and wider afield to Madagascar(Azania)and India.These correlations are then used to interpret the Mesoproterozoic to Neoproterozoic affinity of the rocks and evolution of the region.Detrital zircon samples from the Chewore-Rufunsa and Kacholola(previously referred to as Luangwa-Nyimba)terranes of the SIB yield zircon U-Pb age populations and evolvedε(Hf)(t)values that are similar to the Muva Supergroup found throughout eastern Zambia,primarily correlating with Ubendian-Usagaran(ca.2.05-1.80 Ga)phase magmatism and a cryptic basement terrane that has been suggested to underlie the Bangweulu Block and Irumide Belt.These data suggest that the SIB was depositionally connected to the Congo Craton throughout the Mesoproterozoic.The more eastern Nyimba-Sinda terrane of the SIB(previously referred to as Petauke-Sinda terrane)records detrital zircon ages andε(Hf)(t)values that correlate with ca.1.1-1.0 Ga magmatism exposed elsewhere in the SIB and Irumide Belt.We ascribe this difference in age populations to the polyphase development of the province,where the sedimentary and volcanic rocks of the Nyimba-Sinda terrane accumulated in extensional basins that developed in the Neoproterozoic.Such deposition would have occurred following late-Mesoproterozoic magmatism that is widespread throughout both the Irumide and Southern Irumide Belts,presently considered to have occurred in response to collision between a possible microcontinental mass and the Irumide Belt.This interpretation implies a multi-staged evolution of the ocean south of the Congo Craton during the mid-Mesoproterozoic to late-Neoproterozoic,which ultimately closed during collision between the Congo and Kalahari cratons. | Brandon L.Alessio Alan S.Collins Peter Siegfried Stijn Glorie Bert De Waele Justin Payne Donnelly B.Archibald | 2019 | Geoscience Frontiers2019，10，6： | 0 |
| 16 | Evolving provenance in the Proterozoic Pranhita-Godavari Basin,India显示文摘The Pranhita-Godavari Basin in central eastern India is one of the Proterozoic 'Purana' basins of cratonic India.New geochronology demonstrates that it has a vast depositional history of repeated basin reactivation from the Palaeoproterozoic to the Mesozoic.U-Pb laser ablation inductively coupled plasma mass spectrometry dating of detrital zircons from two samples of the Somanpalli Group—a member of the oldest sedimentary cycle in the valley-constrains its depositional age to ~1620 Ma and demonstrates a tripartite age provenance with peaks at ~3500 Ma,~2480 Ma and ~1620 Ma,with minor age peaks in the Eoarchaean(~3.8 Ga) and at ~2750 Ma.These ages are consistent with palaeocurrent data suggesting a southerly source from the Krishna Province and Enderby Land in East Antarctica.The similarity in the maximum depositional age with previously published authigenic glauconite ages suggest that the origin of the Pranhita-Godvari Graben originated as a rift that formed at a high angle to the coeval evolving late Meosproterozoic Krishna Province as Enderby Land collided with the Dharwar craton of India.In contrast,detrital zircons from the Cycle III Sullavai Group red sandstones yielded a maximum depositional age of 970±20 Ma and had age peaks of ~2550 Ma,~1600 Ma and then a number of Mesoproterozoic detrital zircons terminating in three analyses at ~970 Ma.The provenance of these is again consistent with a southerly source from the Eastern Ghats Orogen and Antarctica.Later cycles of deposition include the overlying Albaka/Usur Formations and finally the late Palaeozoic to Mesozoic Gondwana Supergroup. | Udeni Amarasinghe Asru Chaudhuri Alan S.Collins Gautam Deb Sarbani Patranabis-Deb | 2015 | Geoscience Frontiers2015，6，3： | 0 |
| 17 | 人类基因组计划:大规模生物学的经验显示文摘管理方面的挑战 美国国立卫生研究院(NIH)以同行互相检查的机制被用于人类基因组计划,这种方式既被用来确保研究机构的工作质量,又被作为大规模生物学研究的管理手段。NIH式的资源分配方式既可以资助工作完成地好的测序中心,又可以对达不到标准和经费使用效率的中心给予必要的提醒。仅仅完成预定目标是远远不够的,只有那些不断创新并超额完成测序任务的中心才是成功的。 | Francis S.Collins 胡鸣 | 2003 | 世界科学2003，，7： | 0 |
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