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Generational cultural gaps (assessed as the mismatch between adolescents' ideals and perceptions of the parent–adolescent relationship) were investigated among Chinese youth with immigrant parents and their European American counterparts who have been in the United States for generations and assumingly do not have intergenerational cultural gaps. The authors of the study examined the associations of such generational gaps with adolescents' behavioral problems and whether youth's appreciation of Chinese parent–adolescent relationships (parental devotion, sacrifice, thoughtfulness, and guan) described by the notion of qin would moderate the relationship between discrepancies and youth's adjustment. A total of 634 high school students (M = 15.97 years; 95 and 154 first- and second-generation Chinese American respectively, and 385 European Americans) completed measures of parental warmth, parent–adolescent open communication, qin, and psychological adjustment. The U.S.-born Chinese American adolescents' ideals exceeded perceptions of parents' warmth and open communication to a greater degree than it did for European American adolescents (ps < 0.05). Such discrepancies in parental warmth were related to greater internalizing symptoms for second-generation Chinese American youth than for their European American peers. In addition, for second-generation Chinese, their perceptions of qin, particularly parents' devotion and sacrifice, had stronger moderating effects, diminishing the associations between generational cultural gaps and youth's behavioral problems compared with those of European American and first-generation Chinese youth. Parental thoughtfulness also played a similar beneficial role, but did so for all youth.

To the best of our knowledge, this is the first study reporting prevalence of NSSI defined by suggested DSM-5 criteria among adolescent in rural China. In comparison to finding from the similar samples of adolescents, Chinese rural adolescents seem to have a relative higher prevalence. The potential risk factors for NSSI include female, father's education, Han ethnicity, psychosocial factors and suicide behaviors. More evidence for further understanding of context of the occurrence, improving access to health care utilization, and identifying the role of psychosocial factors and family relationship, is needed for the prevention and management of NSSI.

Amphibolite-facies para-and orthogneisses near Dulan, at the southeast end of the North Qaidam terrane, enclose minor eclogite and peridotite which record ultra-high pressure (UHP) metamorphism associated with the Early Paleozoic continental collision of the Qilian and Qaidam microplates. Field relations and coesite inclusions in zircons from paragneiss suggest that felsic, mafic, and ultramafic rocks all experienced UHP metamorphism and a common amphibolite-facies retrogression. SHRIMP-RG U-Pb and REE analyses of zircons from four eclogites yield weighted mean ages of 449 to 422 Ma, and REE patterns (flat HREE, no Eu anomaly) and inclusions of garnet, omphacite, and rutile indicate these ages record eclogite-facies metamorphism. The coherent field relations of these samples, and the similar range of individual ages in each sample suggests that the ϳ25 m.y. age range reflects the duration of eclogite-facies conditions in the studied samples. Analyses from zircon cores in one sample yield scattered 433 to 474 Ma ages, reflecting partial overlap on rims, and constrain the minimum age of eclogite protolith crystallization. Inclusions of Th ؉ REE-rich epidote, and zircon REE patterns are consistent with prograde metamorphic growth. In the Lu ¨liang Shan, approximately 350 km northwest in the North Qaidam terrane, ages interpreted to record eclogite-facies metamorphism of eclogite and garnet peridotite are as old as 495 Ma and as young as 414 Ma, which suggests that processes responsible for extended high-pressure residence are not restricted to the Dulan region. Evidence of prolonged eclogite-facies metamorphism in HP/UHP localities in the Northeast Greenland eclogite province, the Western Gneiss Region of Norway, and the western Alps suggests that long eclogite-facies residence may be globally significant in continental subduction/collision zones.introduction Ultra-high pressure (UHP) metamorphism, defined by the pressure-temperature conditions of the coesite stability field (P Ͼ 27 kbar, depths Ͼ 80 km), is a product of continental subduction and collision. Since the discovery of metamorphic coesite (Chopin, 1984;Smith, 1984) and diamond (Sobolev and Shatsky, 1990), UHP terranes have been documented from more than 15 localities (for example, Liou and others, 2002). Typically, evidence of UHP metamorphism is preserved as rare mineral inclusions or relict mineral assemblages within host rocks that equilibrated at crustal conditions. Rapid exhumation from UHP conditions is commonly invoked (for example, Gebauer and others, 1997; Cong and others, 2000;Brueckner and van Roermund, 2004) to preserve the unusual UHP assemblages from thermal overprinting (Hacker and Peacock, 1995). Careful geochronological studies, linked to P-T conditions, have documented rapid (cm/a, similar to horizontal plate velocities) exhumation in several localities (for example,

This paper provides further evidence for the ongoing discussion as to whether the Dabie UHPM belt formed in Triassic or Palaeozoic time, and whether the Sulu UHPM belt formed in Triassic or Neoproterozoic time. Combined use of laser Raman spectrometer (LR), cathodoluminescence imaging (CL), and ion probe U-Pb in-situ dating (SHRIMP) provided accurate ages of UHPM from rocks collected from Weihai, NE Sulu UHPM belt. LR was used to identify coesite and other UHP minerals as inclusions in zircon separates from an amphibolized peridotite and an eclogite. CL was used to examine the zoning structure of these zircon, and SHRIMP dating was performed on specific spots on zircon to obtain ages of different geological events. An age of 221 ± 12 Ma was obtained for coesite-bearing zircon from the amphibolized peridotite; an age of 228 ± 29 Ma for eclogite was obtained from the lower intercept of a concordia plot. These ages are interpreted as the time of UHPM in the Weihai region. Ultramafic rocks to the east of Weihai yield a magmatic age at 581 ± 44 Ma. The zircon in the ultramafic rocks possibly also records a thermal event at c. 400 Ma, but no independent geological evidence for this event has been found. The eclogite protolith formed in the Middle Proterozoic (1821 ± 19 Ma), which is similar to the age of country rock gneisses of 1847-1744 Ma. The new geochronological data confirm that UHPM occurred in the Triassic in the Sulu area when subduction took the ultramafic body and the eclogite protolith, together with the adjacent supracrustal rocks, to mantle depths.