Skip to main content

Advertisement

Table 1 Rock-eval pyrolysis, total organic carbon (TOC), and vitrinite reflectance data for the study areas

From: Mechanism of long-standing Cenozoic basin formation in central Hokkaido: an integrated basin study on an oblique convergent margin

Sample ID Depth (m) T max(°C) S 1(mg/g) S 2(mg/g) S 3(mg/g) TOC (wt.%) % Ro
Chinomi-gawa section        
 CH26 533 442 0.05 0.89 0.33 0.96 0.69
 CH01 535 443 0.02 0.61 0.32 1.00 0.78
 CH02 590 434 0.02 0.27 0.14 0.62 0.83
 CH03 613 437 0.02 0.23 0.23 0.57 0.83
 CH05 738 436 0.02 0.33 0.21 0.63 0.73
 CH06 741 439 0.05 0.54 0.21 0.90 0.86
 CH07 773 440 0.02 0.38 0.19 0.93 0.89
 CH08 792 440 0.02 0.26 0.24 0.70 0.82
 CH10 802 438 0.02 0.31 0.22 0.74 0.84