西藏申扎早白垩世花岗岩类:板片断离的证据   总被引：15，自引：10，他引：5  

张亮亮  朱弟成  赵志丹  廖忠礼  王立全  莫宣学 《岩石学报》2011,27(7):1938-1948

拉萨地块中北部地区在~113Ma发生的带状岩浆大爆发事件被认为是南向俯冲的班公湖-怒江洋壳岩石圈板片断离的结果,但缺乏更多的地球化学数据。本文报道的拉萨地块中部申扎地区花岗岩类地球化学数据为这一模型提供了可靠的地球化学证据。申扎花岗岩类包括寄主花岗闪长岩(113Ma),辉长质包体和闪长质包体(111Ma)。申扎早白垩世花岗岩中的寄主岩石与镁铁质包体均属于偏铝质中-高钾钙碱性系列,所有样品均富集大离子亲石元素(如Rb、Ba、U和Th)、亏损高场强元素(如Nb、Ta、Ti和Zr)。花岗闪长质寄主岩和闪长质包体具有高的(⁸⁷Sr/⁸⁶Sr)_i值(0.7121~0.7133),负的ε_Nd(t)值(-10.2~-9.1)及古老的Nd同位素模式年龄(1.90~1.55Ga);辉长质包体具偏低的(⁸⁷Sr/⁸⁶Sr)_i值(0.7067和0.7108),较高的全岩ε_Nd(t)(-2.1和-4.1)值,Nd同位素模式年龄为1.33Ga和1.32Ga。申扎花岗岩类中的辉长质包体具有板内玄武岩亲缘性,这一特征与班公湖-怒江洋壳岩石圈南向俯冲板片在~113Ma左右发生的板片断离有关。申扎花岗岩类是在板片断离背景下,主要由来源于古老拉萨基底物质重熔的熔体与上涌的软流圈地幔物质发生岩浆混合产生的。  相似文献   

Unmasking geographic polarization and clustering: A micro-scalar analysis of partisan voting behavior     

《Applied geography (Sevenoaks, England)》2015

“Geographic polarization”, the spatial concentration of “like” voting behavior, is a phenomenon closely related to “partisan polarization”, the intensification of diametrically ideological positions, is understudied, and is critical to the understanding of current American electoral behavior. To date, few studies have examined geographic polarization, and those that do have done so at the scales of regions, states, and counties. However, local influences operating within areas smaller than counties influence voting behavior and can produce geographic polarization. To address these scalar and methodological shortcomings, this research focuses on the smallest political units, precincts, using a case study of the Greater Cincinnati Metropolitan Area. Presidential election data from 1976 through 2008 were collected by precincts, analyzed using spatial statistics, and mapped to examine evolving geographic polarization over this 32-year period. The results measured at the precinct-scale, suggest an increased concentration of partisan behavior and emphasize a local residential spatial pattern of geographic polarization.  相似文献   

Magmatism During the Exhumation in the Northern Qinghai–Tibet Plateau:Evidence from Granitoids and Enclaves in Dulan area     

JIANG Hongan  MA Changqian  XIONG Fuhao  LIU Bin  HUANG Jian 《《地质学报》英文版》2013,87(Z1):36-36

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东昆仑造山带晚三叠世岩浆混合作用：以和勒冈希里克特花岗闪长岩体为例   总被引：6，自引：2，他引：4       下载免费PDF全文

陈国超  裴先治李瑞保李佐臣裴 磊刘战庆陈有炘刘成军 《中国地质》2013,40(4):1044-1065

东昆仑造山带晚华力西期-印支期花岗质岩石中广泛发育暗色微粒包体.本文以东昆仑东段和勒冈希里克特花岗闪长岩体为例,对暗色微粒包体及其寄主岩进行了详细研究.包体的野外产出特征、形态、结构构造和矿物学特征表明,他们是基性岩浆进入中酸性岩浆快速冷凝结晶的产物,和寄主花岗岩有着相似的稀土元素配分模式,显示轻稀土富集,重稀土亏损,轻重稀土元素分馏明显的特征,微量元素蛛网图也具有明显的相似性,富集大离子亲石元素,亏损高场强元素,反映了岩浆混合作用的特征;LA-ICP-MS锆石U-Pb同位素年代学研究显示,暗色微粒包体的形成年龄为(224.9±4.1)Ma,与寄主岩的同位素年龄值(225±5)Ma在误差范围内一致,表明了在晚三叠世期间东昆仑地区存在着后碰撞阶段壳-幔岩浆混合作用.  相似文献   

And Did the Walls Come Tumbling Down? Ethnic Residential Segregation in Four U.S. Metropolitan Areas 1980-2000     

《Urban geography》2013,34(7):560-581

The initial releases of data from the 2000 U.S. Census allow exploration of the extent of change, if any, in residential segregation in four major cities, where substantial population growth has continued to generate increased ethnic diversity. Using a recently established method of classifying residential areas according to their ethnic composition which facilitates comparative study over time and space, this paper examines segregation trends in Chicago, Los Angeles, New York, and Miami over the period 1980-2000 in the context of recent discussions of the nature of residential patterns there. It finds that though there has been some reduction in the extent of extreme segregation areas that are predominantly either White or African American with consequent greater ethnic mixing at the census tract level, nevertheless cores of extreme segregation remain, and these are being extended with greater segregation of the Hispanic population. Ethnic residential segregation in United States' metropolitan areas attracted much research throughout the 20th century, with each census providing new impetus for mapping and analysis. The 2000 census will be no exception, providing data with which the extent of change can be assessed after a further decade in which discrimination on the grounds of race and color was illegal. This paper provides an initial exploration for four metropolitan areas that have experienced substantial recent multi-ethnic in-migration. Using a method for classifying residential areas designed to facilitate comparative studies over space and time, it explores the extent of desegregation during the previous 20 years for each of the four main census ethnic groups.  相似文献   

Origin of the Miocene porphyries and their mafic microgranular enclaves from Dabu porphyry Cu–Mo deposit,southern Tibet: implications for magma mixing/mingling and mineralization     

《International Geology Review》2012,54(5):571-595

The origin of magmas that are linked to economic mineralization in porphyry deposits formed in continental collisional belts is controversial. In this paper, we studied the mafic microgranular enclaves (MMEs) and their host monzogranite porphyries (HMPs) from the Dabu porphyry Cu–Mo deposit in southern Tibet. Zircon SHRIMP U–Pb ages indicate coeval formation for the MMEs and HMPs in middle Miocene time (~15 Ma). The MMEs have high Mg# (50.7–60.8), low SiO₂ (53.2–62.5 wt.%), and high Cr (95–175 ppm) contents, with positive εHf(t) values ranging from +3.4 to +9.4. These results, along with the presence of phlogopite, suggest that the MMEs were most likely generated by partial melting of a metasomatic lithospheric mantle source region. The HMPs have high Sr/Y (88.2–135.7), La/Yb (25.0–31.9) ratios, and moderate Mg# (46.2–49.3) values. They have the same εHf(t) values (+3.3 to +7.7) with arc-like Palaeogene rocks. The HMPs also show typical arc magma characteristics such as enrichment in LILEs (e.g. Rb, Ba, Sr, and K) and depletion in HFSEs (e.g. Nb, Ta, Ti, Zr, and P). These results suggest a possible origin involving high-pressure remelting of thickened lower crustal arc cumulates related to earlier Neo-Tethyan subduction. The lower crustal arc cumulates dominated by garnet-bearing amphibolite facies could be the potential copper sources of the Dabu porphyry Cu–Mo deposit. Underplating of the mantle-derived mafic magmas could have provided heat input for melting of the hydrous lower crust. Reaction between the mafic and felsic magmas might have further increased Cu concentrations and contributed to subsequent mineralization.  相似文献   

Petrogenesis and tectonic implications of ultrapotassic microgranitoid enclaves in Late Triassic arc granitoids,Qinling orogen,central China     

《International Geology Review》2012,54(2):208-226

The origin of microgranitoid enclaves in granitic plutons has long been debated (hybrid magma blobs vs. refractory restites or cognate fragments). This article presents detailed petrography, SHRIMP zircon U–Pb chronology, bulk-rock major and trace element analyses, and Sr–Nd isotope and in situ zircon Hf isotopic geochemistry for microgranitoid enclaves within two Late Triassic granitic plutons in the Qinling orogen. Zircon U–Pb dating shows that the enclaves formed during the Carnian (222.5 ± 2.1 to 220.7 ± 1.9 Ma) coeval with their host granitoids (220.0 ± 2.0 to 218.7 ± 2.4 Ma). Field and petrological observations (e.g. double enclaves, xenocrysts, acicular apatite, and poikilitic K-feldspar or quartz) suggest that the enclaves are globules of a mantle-derived more mafic magma that was injected into and mingled with the host magma. The enclaves are mainly ultrapotassic, distinct from the host granitoids that have high-K calc-alkaline bulk-rock compositions. Although the enclaves have closely similar bulk-rock Sr–Nd isotope [initial ⁸⁷Sr/⁸⁶Sr?=?0.7046–0.7056, ?_Nd (T)?=?–0.3 to –5.0] and in situ zircon Hf isotope [?_Hf (T)?=?–1.5 to?+2.9] ratios as the granitoids [initial ⁸⁷Sr/⁸⁶Sr?=?0.7042–0.7059, ?_Nd (T)?=?–0.6 to –6.3, ?_Hf (T)?=?–2.2 to?+1.6], chemical relationships including very different bulk-rock compositions at a given SiO₂ content lead us to interpret the isotopic similarities as reflecting similar but separate isotopic source rocks. Detailed elemental and isotopic data suggest that the enclaves and the host granitoids were emplaced in a continental arc environment coupled with northward subduction of the Palaeo-Tethyan oceanic crust. Partial melting of subducted sediments triggered by dehydration of the underlying igneous oceanic crust, with melts interacting with the overlying mantle wedge, formed high-K calc-alkaline granitic magmas, whereas partial melting of diapiric phlogopite-pyroxenites, solidified products of the same subducting sediment-derived melts, generated ultrapotassic magmas of the microgranitoid enclaves. Our new data further confirm that in the Late Triassic time the Qinling terrane was an active continental margin rather than a post-collisional regime, giving new insights into the tectonic evolution of this orogen.  相似文献   

Geochronology of the Gabbro–mafic Microgranular Enclaves–granite Associations in the Gejiu District, Yunnan Province and Their Geodynamic Significance     

CHENG Yanbo  MAO Jingwen 《《地质学报》英文版》2012,86(3):748-761

Many igneous rocks distribute in Gejiu tin polymetallic ore-field at Yunnan province, rocks including basalt, gabbro, mafic microgranular enclaves, granites (porphyritic granite and equigranular granite) and akaline rocks. The ages of the granites and akaline rocks which are considered to have genetic connecting with the mineralization have been comfirmed, but the gabbro-mafic microgranular enclaves-granite assemblage’s ages are still unknown. By means of LA-ICP-MS zircon U-Pb dating, the data of Shenxianshui equigranular granite, the mafic microgranular enclave in Jiasha area, the host rock of the mafic microgranular enclaves and the Jiasha gabbro are around ~80 Ma. Besides the above mentioned data, a group of new ages at ~30 Ma were discovered in this study, which is from gabbro and mafic microgranular enclaves. Based on the previous data and the new data gained this time, we suggest the major geochronology framework of the magmatism and mineralization events in Gejiu area is ~80 Ma, which is consistent with the Late Cretaceous magmatism and mineralization events in the whole southeast Yunnan and west Guangxi area and they were suggested to belong to the same geotectonic setting in late Yenshannian. And the new ages of the ~30 Ma obtained in this study is considered to represent a responding to the complicate tectonic evolution history of the Tibetan orogenic events in Cenozoic.  相似文献   

Social Network Approach to Understand the Ethnic Economy: A Theoretical Discourse<Superscript>1</Superscript>     

Arent?GreveEmail author  Janet?W.?Salaff 《GeoJournal》2005,64(1):7-16

In this paper we suggest how social network analysis, in contrast to looking at physical space, can be used to trace the social and economic location of ethnic enclaves. Taking skilled workers immigrating to Canada from China as an example, we analyze critically how split labor market theories describe materialist and structural factors that determine immigrants’ limited options. Cultural theories play up immigrants’ interest in using their cultural resources to pull themselves ahead. We propose that social network analysis as a single framework can bring together elements from materialist–structural and cultural theories. The position of people and firms in these networks gives us a view of the kinds of jobs immigrants get and the businesses they set up. To understand the ethnic economy, we discuss how networks of social and economic relations intersect each other. By seeing the ethnic economy embedded in social networks, we can provide a more general explanation of the social space of the ethnic economy in contrast to its physical location. We use three cases of ethnic entrepreneurs to illustrate how the social and economic relations locate their businesses in the enclave and how they are also linked to the mainstream economy. ¹This paper has benefitted from the critical clarifications of Chiu Luk and an anonymous reviewer, and the talented editing of Allen Sutterfield. Lynn Xu Liping helped on an earlier draft.  相似文献   

Petrogenesis of granitoid rocks at the northern margin of the Eastern Ghats Mobile Belt and evidence of syn-collisional magmatism     

S.?BhattacharyaEmail author  Rajib?Kar  S.?Moitra 《Journal of Earth System Science》2004,113(4):543-563

The northern margin of the Eastern Ghats Mobile belt against the Singhbhum craton exposes granitic rocks with enclaves from both the high-grade and low-grade belts. A shear cleavage developed in the boundary region is also observed in these granitoids. Field features and petrography indicate syn-tectonic emplacement of these granitoids. Petrology-mineralogy and geochemistry indicate that some of the granitoids are derived from the high-grade protoliths by dehydration melting. Others could have been derived from low-grade protoliths. Moreover, microstructural signatures in these granitoids attest to their syn-collisional emplacement.  相似文献