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		题名	作者	年代	出处	被引量
	1	Concentration phase diagram of BaxSr1-xTiO3 solid solutions 显示文摘	Shirokov V B TorgashevV I Bakirov A A	2006	Phys Rev B2006，73，10：	1
	2	Quartz pseudomorph after coesite in garnet from a garnet chloritoid-talc schist,nortern Tiensha,Kirghiz,USSR显示文摘	Tagiri M Bakirov A	1990	Proc Japan Acad1990，66，：	1
	3	Climate change and glaciers of the Tien-Shan for the last 100 years显示文摘	Podrezov O A Dikih N A Bakirov K B		0，，03：	1
	4	Measuring and testing independence by correlation of distances显示文摘	Sz6kely G J Rizzo M L Bakirov N K	2007	The Annals of Applied Statistics2007，35，：	1
	5	Mineral parageneses and metamorphic P-T paths of ultrahigh-pressure eclogites from Kyrgyzstan Tien-Shan显示文摘	Tagiri M Yano T Bakirov A	1995	The Island Arc1995，4，：	1
	6	Measuring and Testing Depen-dence By Correlation of Distances显示文摘	SzekelyG J Rizzo M L Bakirov N K	2007	The Annals of Statistics2007，35，6：	1
	7	Measuring and testing independence by correlation of distances显示文摘	Szkely G J Rizzo M L and Bakirov N K	2007	The Annals of Statistics2007，35，6：	1
	8	Brownian distance covariance显示文摘	Szkely G J Pdzzo M L and Bakirov N K	2009	The Annals of Applied Statistics2009，3，4：	1
	9	Petrology of metamorphic rocks from the Atbashy complex,Southern Tien-Shan,Kyrgyzstan显示文摘The high-to ultrahigh-pressure metamorphic rocks of the Atbashy complex were petrologically investigated. The eclogites of the Choloktor Formation show a prograde evolution from epidote-blueschist facies(P = 17-21 kbar and T = 450-515 ℃) to peak eclogite-UHP conditions(P = 26-29 kbar and T = 545-615 ℃) with a subsequent epidote-amphibolite and greenschist facies overprint. The micaschists of the Choloktor Formation also show a clockwise P-T path from blueschist/epidote-blueschist facies conditions through peak eclogite facies conditions(P = 21-23 kbar and T = 530-580 ℃) to retrograde epidote-amphibolite and greenschist facies stages. A comparison of the P-T paths in the eclogites and mica-schists of Choloktor Formation reveal that they may have shared their P-T history from peak to retrograde stages. The mica-schists of the Atbashy Formation record peak metamorphism of P = 10-12 kbar and T = 515-565 ℃, which indicates that the highest grade of regional metamorphism in the Atbashy Ridge was epidote-amphibolite facies.The newly obtained P-T conditions for the mica-schists of Choloktor Formation indicate that sheets of sedimentary rocks were brought to great depths along the subduction zone and they metamorphosed under eclogite facies HP conditions. The eclogite blocks were amalgamated with mica-schists of Choloktor Formation in the eclogite facies HP conditions and together they experienced isothermal decompression to ~40 km. During this path, the eclogites and mica-schists of Choloktor Formation docked with mica-schists of Atbashy Formation at 10-12 kbar and 515-565 ℃, and from this depth(~40 km) the whole sequence was exhumed together. These new results improve our understanding of high-pressure metamorphism in subduction-related accretionary prism zones and the exhumation processes of deeply-seated rocks in the Atbashy HP-UHP complex.	Maksatbek Satybaev Lin Ding Akira Takasu Apas Bakirov Kadyrbek Sakiev Fulong Cai Rustam Orozbaev Azamat Bakirov Janybek Baslakunov	2018	Geoscience Frontiers2018，9，6：	1
	10	Comparison theorem for distribution of quadratic forms of Gaussian vectors显示文摘	Bakirov N K	1995	Theory Probab Appl1995，40，：	1
	11	Extremal probabilities for Gaussian quadratic forms显示文摘	Székely G J Bakirov N K	2003	Probab Theory Relat Fields2003，126，：	1
	12	Concentration phase diagram of Ba~Srl,TiO3 solid solutions 显示文摘	Shirokov V B Torgashev V I Bakirov A A	2006	Phys Rev B2006，73，10：	1
	13	Mineral para geneses and meta- morphic P-T paths of ultrahigh-pressure eclogites from Kyrghyas tan Tian-Shan显示文摘	Tagiri M ano T Bakirov A	1995	The Island Arc1995，4，：	1

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