Magmatic hydrothermal fluid genesis of zeolite in the Paleogene Kongdian Formation of Zaoyuan oilfield, Bohai Bay Basin, China

HAN Guomeng,WANG Li,XIAO Dunqing,LOU Da,XU Muyue,ZHAO Yonggang,PEI Yanlu,GUO Xiaowen,TENG Jiancheng,HAN Yuanjia

Table 3 Calculation results of overlapping peak resolving of Raman spectroscopy.

Point No. Fitted peak area R2 Tempera- ture/°C D1 G D2 B-1 1 181 190 354 512 159 528 0.70 331 B-2 1 597 010 498 247 381 846 0.64 354 B-3 1 571 720 595 634 193 937 0.67 345 B-4 1 167 350 389 088 197 561 0.67 345 B-5 1 022 100 384 796 85 618 0.68 336 G-1 907 061 281 262 85 783 0.71 324 G-2 478 970 174 797 42 976 0.69 335 G-3 607 146 253 280 39 774 0.67 341 G-4 687 661 295 002 84 192 0.64 354 W-1 1 107 360 366 427 89 622 0.71 326 W-2 1 072 480 403 303 63 148 0.70 331 W-3 1 082 940 421 632 72 396 0.69 335 W-4 735 433 289 911 79 265 0.67 345 W-5 911 783 349 688 60 350 0.69 334