南秦岭刘岭群砂岩碎屑锆石LA-ICP-MS U-Pb年龄及其构造意义   总被引：7，自引：0，他引：7  

陈龙耀  罗玉凌  刘晓春  曲玮  胡娟 《地质通报》2014,33(9):1363-1378

秦岭造山带的构造演化是理解华北与扬子陆块缝合过程的关键,位于商丹断裂带以南的刘岭群是揭示秦岭造山带晚古生代构造演化历史的重要窗口。采用LA-ICP-MS对刘岭群3个变质砂岩样品中的碎屑锆石进行了U-Th-Pb同位素测定,获得最年轻的一组年龄区间为377~395Ma,主要年龄峰值约为442Ma、780~850Ma和900~970Ma,表明刘岭群沉积时代可以持续到晚泥盆世,物质来源于北秦岭构造带。结合刘岭群北侧武关杂岩的最新研究成果可以确定,刘岭群和武关杂岩共同构成了华北陆块南缘中—晚泥盆世弧前盆地的沉积序列,暗示古秦岭洋的最终闭合发生在泥盆纪之后,而华北与扬子陆块碰撞的主缝合线应位于刘岭群的南侧。  相似文献   

中国沙漠的碎屑长石矿物与冰期风尘示踪     

李娟  何同 《高校地质学报》2021,27(3):366-374

文章采用了新型自动矿物相识别技术（INCA Mineral）对中国北方10个沙漠盆地以及蒙古戈壁沉积物的碎屑长石开展了矿物定量研究。钾长石/钠长石和钙质斜长石/石英的比值指示了沙漠沉积物的长石矿物含量特征,表现出显著的地球化学区域分布特证。沿着青藏高原北部边缘分布的塔克拉玛干、柴达木、腾格里、巴丹吉林与毛乌素沙漠的沉积物中两种长石矿物比值均较低;中亚造山带以北的古尔班通古特、蒙古戈壁、浑善达克、呼伦贝尔和科尔沁沙漠的沉积物中两种长石矿物指标均具有较高值。长石矿物含量特征揭示的“两单元”区域分布结果,可以由过去采用Nd-Sr-Hf同位素示踪结果来验证。东亚沙漠长石含量的二元空间分布特征,支持了构造成山控制盆地沉积物矿物成分的假说。黄土高原末次冰期黄土的长石含量特征,与青藏高原北缘的长石分布特征一致,该区域可能是末次冰期黄土高原物质的主要来源,但也并不排除中亚造山带物质通过远距离搬运传输对末次冰期风尘的贡献。  相似文献   

Detrital zircon U?Pb ages,Hf isotopes and tectonic implications for Palaeozoic sedimentary rocks from the Xing‐Meng orogenic belt,middle‐east part of inner Mongolia,China     

Dapeng Li  Yuelong Chen  Zhong Wang  Kejun Hou  Changzheng Liu 《Geological Journal》2011,46(1):63-81

The Xing‐Meng Orogenic Belt is the eastern extension of the Central Asian Orogenic Belt that marks the boundary between the North China Block and the Siberian Block. Studies of zircon U Pb ages and Hf isotopic compositions show that four clastic sedimentary rock samples from different parts of the regional stratigraphic sequence were deposited at different ages, none earlier than Mid‐ or Early Silurian. Two sedimentary rocks were deposited during or after the Early Permian. Almost all zircons are of igneous origin. In Silurian and Devonian sediments, zircons show several modal age peaks, and in Permian sediments, zircons show a unimodal age peak. Based on the zircon age distribution of sedimentary rocks versus known ages from exposed rocks of the potential source regions, most of the zircons were derived from the Xing‐Meng Orogen itself. A few came from the South Mongolian microcontinent or the Siberia Block, but none came from the North China Block. The zircons of a biotite‐plagioclase paragneiss in Xilinhot have similar provenance to the sediments and were deposited during or after the Middle Devonian. Similarities between zircon age spectra and events in underlying rocks of sedimentary origin show that the sediments lie at their deposition site north of the Solonker suture zone because north‐dipping subduction and elevation blocked deposition of material from farther afield. Hf isotope compositions show the crustal accretion stages of the provenance areas during the Meso‐ to Neoarchaean, Palaeoproterozoic and Early and Late Palaeozoic. A two‐component mixing calculation based on Hf isotopes shows the large scale of the crustal accretion event of the region. Copyright © 2010 John Wiley & Sons, Ltd.  相似文献   

鄂尔多斯盆地西南部汭水河地区上三叠统碎屑锆石U Pb年代学特征及其地质意义   总被引：7，自引：0，他引：7  

宋立军  陈隽璐  张英利  刘池洋  吴冲龙  张小浩 《地质学报》2010,84(3):370-386

鄂尔多斯盆地西南部延长组物源及其演化是进行区域原盆恢复和认识区域构造演化及华北克拉通西部破坏的关键。本文以鄂尔多斯盆地西南部汭水河地区晚三叠世延长组砂岩为研究对象,采用锆石LA-ICP-MS测年方法,通过砂岩样品中碎屑锆石U-Pb年龄及其变化,结合区域背景及古水流资料,系统地研究了盆地西南部延长组物源及其演化。研究认为,晚三叠世早期(231～225Ma),盆地西南部延长组沉积物源主要为盆地东北部阜平杂岩及盆地北部的海西期岩浆岩,部分搬运来的物质与来自秦祁造山带的剥蚀物质一起经宝鸡—武都裂陷槽流入松潘—甘孜地区;晚三叠世中期(225～218Ma),来自秦岭造山带的挤压开始增强,盆地西南部延长组地层中来自南缘秦岭造山带的物源开始增加,盆地西南部沉积物源开始与松潘—甘孜地区出现明显差别,宝鸡—武都裂陷槽开始关闭;至晚三叠世晚期(218～210Ma),秦岭与祁连造山带完成拼贴,宝鸡—武都裂陷槽最终完全关闭。  相似文献   

西藏比如盆地碎屑锆石LA-ICP-MS U-Pb测年及其地质意义   总被引：1，自引：0，他引：1  

张士贞  向树元  万俊  毛鑫 《地质科技情报》2010,29(5)

对比如盆地中上侏罗统和下白垩统地层中采集的4个砂岩样品的碎屑锆石进行了LA-ICP-MSU-Pb测年,并将其结果与前人对盆地两侧地质体的测试年龄信息进行对比,据此得出样品405-3物源为盆地北侧喀喇昆仑—南羌塘陆块,其他3个样品物源均来自于盆地南侧的冈底斯—拉萨陆块。通过对比分析认为样品405-3中几组较老的锆石年龄是对羌塘盆地存在结晶基底并遭受后期多期变质变形的肯定。样品417-7,424-1及429-1的年龄既反映了600～500Ma的泛非期活动年龄数据,又显示了拉萨地块存在的中新元古代基底的年龄信息。  相似文献   

盆地沉积物示踪源区山脉隆升剥露的几种方法   总被引：12，自引：0，他引：12  

王岳军  范蔚茗  林舸 《地质科技情报》1999,18(2):85-89

简要介绍了盆地沉积物示踪山脉隆升剥蚀的几种方法并给以实例分析。与造山 隆升过程相伴生的沉积盆地记录了造山带隆升的许多宝贵信息,利用盆地沉积物反演原区背景常局限于盆地沉积物碎屑组分、副（重）矿物组合及元素地球化学特征的变化,近年国外已开始利用盆地沉积物中颗粒错石Ｕ－Ｐｂ年龄谱、Ｎｄ同位素组成、矿物（如黑云母、磷灰石等）热年代学方法示踪盆地沉积物物源性质及物源贡献比例,山脉构造热事件及山脉升剥蚀速率等  相似文献   

Inversion of provenance data and sediment load into spatially varying erosion rates     

Fien De Doncker  Frédéric Herman  Matthew Fox 《地球表面变化过程与地形》2020,45(15):3879-3901

Sediment fingerprinting methods aim to determine the relative contribution of different source areas in detrital sediments based on natural properties – fingerprints – of the source areas. Here, we use U/Th–Pb age signatures as fingerprints, assuming that the age signal is not altered during erosion–transportation–deposition events, and given that recent technological advances enable precise dating of large amounts of grains. We introduce a formal inversion method that allows to disentangle the amalgamation of source contributions in detrital zircon data and enables to convert this information into an erosion rate map starting from the spatial distribution of zircon age signatures. Relying on the least-squares method and using prior and covariance information to deal with non-uniqueness, we show, using synthetic and natural examples, that we are able to retrieve erosion rate patterns of a catchment when the age distribution and zircon fertility for each source area are well known. Moreover, we show that not only zircon age fingerprints but also other tracers such as mineral content can be used. Furthermore, we found that adding data from samples taken at the outlet of tributaries improves the estimation of erosion rate patterns. We conclude that the least squares inverse model applied to detrital data has great potential for investigating erosion rates. © 2020 John Wiley & Sons, Ltd.  相似文献   

Late Cretaceous uplift history of the Cretaceous volcanic arc in Southwest Japan: Provenance analysis of the Yuasa–Aridagawa basin based on U–Pb zircon ages          下载免费PDF全文

Ryosuke Shunori  Makoto Takeuchi  Koshi Yamamoto 《Island Arc》2018,27(4)

The Ryoke Metamorphic complex has undergone low‐P/T metamorphism and was intruded by granitic magmas around 100 Ma. Subsequently, the belt was uplifted and exposed by the time deposition of the Izumi Group began. The tectonic history of uplift, such as the timing and processes, are poorly known despite being important for understanding the spatiotemporal evolution of the Ryoke Metamorphic Belt. U–Pb zircon ages from sedimentary rocks in the forearc and backarc basins are useful for constraining uplift and magmatism in the provenance. U–Pb dating of detrital zircons from 12 samples (four sandstones and eight granitic clasts) in the Yuasa–Aridagawa basin, a Cretaceous forearc basin in the Chichibu Belt of Southwest Japan, gave mostly ages of 60–110 Ma. Granitic clasts contained in conglomerate suggest that granitic intrusions predate the formation of Coniacian and Maastrichtian conglomerate. Emplacement ages of granitic bodies originated from granitic clasts in Coniacian conglomerate are (110.2 ±1.3) Ma, (106.1 ±1.8) Ma, (101.8+5.8–3.8) Ma, and (95.3 ±1.4) Ma; for granitic clasts in Maastrichtian conglomerate, (89.6 ±1.8) Ma, (87.3+2.4–1.8) Ma, (85.7 ±1.2) Ma, and (82.7 ±1.2) Ma. The results suggest that detrital zircons in the sandstones were mainly derived from volcanic eruptions contemporaneous with depositional age, and plutonic rocks of the Ryoke Metamorphic Belt. Zircon ages of the granitic clast samples also indicate that uplift in the provenance began after Albian and occurred at least during the Coniacian to Maastrichtian. Our results, together with the difference of provenance between backarc and forearc basins suggest that the southern marginal zone of the Ryoke Metamorphic Belt was uplifted and supplied a large amount of clastic materials to the forearc basins during the Late Cretaceous.  相似文献   

Diverse protolith ages for the Mindoro and Romblon Metamorphics (Philippines): Evidence from single zircon U–Pb dating          下载免费PDF全文

Ulrich Knittel  Monika Walia  Shigeyuki Suzuki  Carla B. Dimalanta  Graciano P. Yumul Jr. 《Island Arc》2017,26(1)

Within the north‐eastern part of the Palawan Continental Terrane, which forms the south‐western part of the Philippine archipelago, several metamorphic complexes are exposed that are considered to be rifted parts of the Asian margin in South‐East China. The protolith age(s) and correlations of these complexes are contentious. The largest metamorphic complex of the Palawan Continental Terrane comprises the Mindoro Metamorphics. The north‐eastern part of this metamorphic complex has recently been found to be composed of protoliths of Late Carboniferous to Late Permian protolith age. However, meta‐sediments exposed at the westernmost tip and close to the southern boundary of the exposure of the Mindoro Metamorphics contain detrital zircons and with U–Pb ages, determined by LA–ICP–MS, in the range 22–56 Ma. In addition, zircons as young as 112 Ma were found in a sample of the Romblon Metamorphics in Tablas. As the youngest detrital zircons provide an upper age limit for the time of deposition in meta‐sediments, these results suggest that the Mindoro and Romblon Metamorphics comprise protoliths of variable age: Late Carboniferous to Late Permian in NE Mindoro; Eocene or later in NW Mindoro; Miocene at the southern margin of the Mindoro metamorphics; and Cretaceous or later on Tablas. The presence of non‐metamorphic sediments of Late Eocene to Early Oligocene age in Mindoro (Lasala Formation), which are older than the youngest metasediments, suggests that metamorphism of the young meta‐sediments of Mindoro is the result of the collision of the Palawan Continental terrane with the Philippine Mobile Belt in Late Miocene. Similarities of the age spectra of zircons from the Eocene to Miocene metamorphics with the Eocene to Early Miocene Lasala Formation suggest that the protoliths of the young metamorphics may be equivalents of the Lasala Formation or were recycled from the Lasala Formation.  相似文献   

Controls on Early Cretaceous desert sediment provenance in south-west Gondwana,Botucatu Formation (Brazil and Uruguay)     

Gabriel Bertolini  Juliana C. Marques  Adrian J. Hartley  Atila A. S. Da-Rosa  Claiton M. S. Scherer  Miguel A. S. Basei  José C. Frantz 《Sedimentology》2020,67(5):2672-2690

The Lower Cretaceous Botucatu Formation records the development of widespread dry–aeolian desert sedimentation throughout the Paraná Basin in south-west Gondwana. To reconstruct the provenance of the aeolian sediment, petrography, granulometric analysis, U-Pb detrital zircon ages have been determined from along the southern basin margin in Rio Grande do Sul state (southern Brazil) and Uruguay (Tacuarembó region). The dataset reveals a mean composition Qt₈₉F₈L₃, comprising very fine to medium-grained quartozose and feldspatho-quartzose framework. Heavy mineral analysis reveals an overall dominance of zircon, tourmaline and rutile grains (mean ZTR_0.84) with sporadic garnet, epidote and pyrolusite occurrences. The detrital zircon U-Pb ages are dominated by Cambrian to Neoproterozoic (515 to 650 Ma), Tonian to Stenian (900 to 1250 Ma) and Orosirian to Rhyacian (1.8 to 2.2 Ga) material. The detrital zircon dataset demonstrates a significant lateral variation in sediment provenance: Cambrian to Neoproterozoic detrital zircons dominate in the east, while Tonian to Stenian and Orosirian to Rhyacian ages predominate in the west of the study area. Sandstones are quartz-rich with dominantly durable zircon, tourmaline and rutile heavy mineral suite, with subtle but statistically significant along-strike differences in heavy mineral populations and detrital mineralogy which are thought to record local sediment input points into the aeolian system. The similar age spectra of Botucatu desert with proximal Paraná Basin units, the predominance of quartzose, and zircon, tourmaline and rutile components, suggests that recycling is the mechanism responsible for the erg feeding.  相似文献