öλÔÓéÀֵǼÈë¿ÚÏÂÔØ

µ¼Ê¦ÐÕÃû£ºÍõ¶ÔÐË
ÐÔ±ð£ºÄÐ
ÈËÆøÖ¸Êý£º60

ËùÊôԺУ£ººÓ±±µØÖÊ´óѧ
ËùÊôԺϵ£º×ÊԴѧԺ
Ö°³Æ£º½²Ê¦
µ¼Ê¦ÀàÐÍ£ºË¶µ¼
ÕÐÉúöλÔÓéÀֵǼÈë¿ÚÏÂÔØ£º¿óÎïѧ¡¢ÑÒʯѧ¡¢¿ó´²Ñ§
Ñо¿ÁìÓò£º ÑÒʯѧ¡¢ÑÒ½¬ÑÒÑÒʯѧ¡¢ÑÒʯµØÇò»¯Ñ§
Ñо¿ÁìÓò£º ÑÒʯѧ¡¢ÑÒ½¬ÑÒÑÒʯѧ¡¢ÑÒʯµØÇò»¯Ñ§ [ÊÕÆð]




ͨѶ·½Ê½ :
°ì¹«µç»°£º**
µç×ÓÓʼþ£ºwangdx0319@163.com


¿ÆÑй¤×÷ :
ÔÚ¹úÄÚÍâºËÐÄÆÚ¿¯ÉÏ·¢±íѧÊõÂÛÎÄÇé¿ö:Õ㶫Ôç°×ÛÑÊÀÑÒ½¬»ìºÏ×÷ÓÃ:вýС½«ÑÒÌåU-PbÄê´úѧ¼°µØÇò»¯Ñ§Ö¤¾Ý£¬ÑÒʯѧ±¨£¬¹úÄÚ£¬SCI 29£¨11£©£¬ÅÅÃû1£»ËÉÁÉÅèµØ±±²¿ÍíÖÐÉú´úÖÐËáÐÔ»ðɽÑÒµØÇò»¯Ñ§ÌØÕ÷¼°³ÉÒò̽ÌÖ£¬¿óÎïÑÒʯ£¬¹úÄÚ£¬SCI 33£¨3£©£¬ÅÅÃû1£»ÕãÖкóɽµê»¨¸Ú°ßÑÒÌåµÄLA-ICP-MSï¯Ê¯U-Pb¶¨Äê¡¢ï¯Ê¯HfͬλËؼ°ÆäµØÖÊÒâÒ壬¿óÎïÑÒʯ£¬¹úÄÚ£¬SCI 35£¨1£©£¬ÅÅÃû1£»ËÉÁÉÅèµØÐì¼ÒΧ×ÓÖÐÉú´ú»ðɽÑÒÐγɻ·¾³£¬×ÊÔ´»·¾³Ó빤³Ì£¬¹úÄÚ£¬ISTP£¬23£¨3£©£¬ÅÅÃû1£»Õã±±ÉÜÐ˵ØÇøÐÂÔª¹Å´úÔçÆÚÂÁÖÊ»¨¸ÚÑÒï¯Ê¯LA-ICP-MS U-Pb¶¨Äê¡¢ÑÒʯµØÇò»¯Ñ§¼°Æä³ÉÒòÌÖÂÛ£¬¿óÎïÑÒʯ£¬¹úÄÚ£¬SCI 34£¨3£©£¬ÅÅÃû1£»ÕãÖеØÇøÍíÙªÂÞÊÀ»¨¸Ú°ßÑÒLA-ICP-MS ï¯Ê¯U-PbÄêÁä¡¢µØÇò»¯Ñ§ÌØÕ÷¼°ÆäµØÖÊÒâÒ壬ÖйúµØÖÊ£¬¹úÄÚ£¬SCI 42£¨6£©£¬ÅÅÃû1£»Crust¨Cmantle interaction triggered by oblique subduction of the Pacific plate:geochronological,geochemical,and Hf isotopic evidence from the Early Cretaceous volcanic rocks of Zhejiang Province,south:International Geology Review£¬¹úÍ⣬ISTP 56(14)£¬ÅÅÃû3£»Õ㶫ÄÏÍíÖÐÉú´ú»¨¸ÚÑÒµÄï¯Ê¯UPbÄê´úѧ¡¢µØÇò»¯Ñ§¼°ÆäµØÖÊÒâÒå ¼ªÁÖ´óѧѧ±¨£¨µØÇò¿Æѧ°æ£©£¬¹úÄÚ£¬EI SCI£¬£¨3£©£¬ÅÅÃû3¡£