. | Disc-dominated . | Bulge-dominated . | B + D . |
---|---|---|---|
This work (HLSy2) | |$29\%^{+12}_{-10}$| | |$71\%^{+5}_{-19}$| | 0%+11 |
This work (QSO2) | |$31\%^{+9}_{-9}$| | |$69\%^{+6}_{-13}$| | 0%+7 |
Dunlop et al. (2003) (RL-QSO1) | 100%−16 | ||
Dunlop et al. (2003) (RQ-QSO1) | |$15\%^{+15}_{-6}$| | |$85\%^{+6}_{-15}$| | |
Floyd et al. (2004) (QSO1) | |$18\%^{+11}_{-7}$| | |$76\%^{+8}_{-13}$| | |$6\%^{+11}_{-3}$| |
Falomo et al. (2014) (QSO1) | |$42\%^{+3}_{-3}$| | |$37\%^{+3}_{-3}$| | |$21\%^{+3}_{-3}$| |
Cales et al. (2011) (QSO1) | |$24\%^{+9}_{-7}$| | |$72\%^{+5}_{-13}$| | |$4\%^{+8}_{-1.4}$| |
Greene et al. (2009) (QSO2) | |$27\%^{+19}_{-9}$| | |$73\%^{+9}_{-17}$| | |
Wylezalek et al. (2016) (QSO2) | |$10\%^{+11}_{-4}$| | |$90\%^{+4}_{-11}$| | |
Inskip et al. (2010) (NLRG) | |$6\%^{+11}_{-3}$| | |$88\%^{+1}_{-17}$| | |$6\%^{+11}_{-3}$| |
. | Disc-dominated . | Bulge-dominated . | B + D . |
---|---|---|---|
This work (HLSy2) | |$29\%^{+12}_{-10}$| | |$71\%^{+5}_{-19}$| | 0%+11 |
This work (QSO2) | |$31\%^{+9}_{-9}$| | |$69\%^{+6}_{-13}$| | 0%+7 |
Dunlop et al. (2003) (RL-QSO1) | 100%−16 | ||
Dunlop et al. (2003) (RQ-QSO1) | |$15\%^{+15}_{-6}$| | |$85\%^{+6}_{-15}$| | |
Floyd et al. (2004) (QSO1) | |$18\%^{+11}_{-7}$| | |$76\%^{+8}_{-13}$| | |$6\%^{+11}_{-3}$| |
Falomo et al. (2014) (QSO1) | |$42\%^{+3}_{-3}$| | |$37\%^{+3}_{-3}$| | |$21\%^{+3}_{-3}$| |
Cales et al. (2011) (QSO1) | |$24\%^{+9}_{-7}$| | |$72\%^{+5}_{-13}$| | |$4\%^{+8}_{-1.4}$| |
Greene et al. (2009) (QSO2) | |$27\%^{+19}_{-9}$| | |$73\%^{+9}_{-17}$| | |
Wylezalek et al. (2016) (QSO2) | |$10\%^{+11}_{-4}$| | |$90\%^{+4}_{-11}$| | |
Inskip et al. (2010) (NLRG) | |$6\%^{+11}_{-3}$| | |$88\%^{+1}_{-17}$| | |$6\%^{+11}_{-3}$| |
. | Disc-dominated . | Bulge-dominated . | B + D . |
---|---|---|---|
This work (HLSy2) | |$29\%^{+12}_{-10}$| | |$71\%^{+5}_{-19}$| | 0%+11 |
This work (QSO2) | |$31\%^{+9}_{-9}$| | |$69\%^{+6}_{-13}$| | 0%+7 |
Dunlop et al. (2003) (RL-QSO1) | 100%−16 | ||
Dunlop et al. (2003) (RQ-QSO1) | |$15\%^{+15}_{-6}$| | |$85\%^{+6}_{-15}$| | |
Floyd et al. (2004) (QSO1) | |$18\%^{+11}_{-7}$| | |$76\%^{+8}_{-13}$| | |$6\%^{+11}_{-3}$| |
Falomo et al. (2014) (QSO1) | |$42\%^{+3}_{-3}$| | |$37\%^{+3}_{-3}$| | |$21\%^{+3}_{-3}$| |
Cales et al. (2011) (QSO1) | |$24\%^{+9}_{-7}$| | |$72\%^{+5}_{-13}$| | |$4\%^{+8}_{-1.4}$| |
Greene et al. (2009) (QSO2) | |$27\%^{+19}_{-9}$| | |$73\%^{+9}_{-17}$| | |
Wylezalek et al. (2016) (QSO2) | |$10\%^{+11}_{-4}$| | |$90\%^{+4}_{-11}$| | |
Inskip et al. (2010) (NLRG) | |$6\%^{+11}_{-3}$| | |$88\%^{+1}_{-17}$| | |$6\%^{+11}_{-3}$| |
. | Disc-dominated . | Bulge-dominated . | B + D . |
---|---|---|---|
This work (HLSy2) | |$29\%^{+12}_{-10}$| | |$71\%^{+5}_{-19}$| | 0%+11 |
This work (QSO2) | |$31\%^{+9}_{-9}$| | |$69\%^{+6}_{-13}$| | 0%+7 |
Dunlop et al. (2003) (RL-QSO1) | 100%−16 | ||
Dunlop et al. (2003) (RQ-QSO1) | |$15\%^{+15}_{-6}$| | |$85\%^{+6}_{-15}$| | |
Floyd et al. (2004) (QSO1) | |$18\%^{+11}_{-7}$| | |$76\%^{+8}_{-13}$| | |$6\%^{+11}_{-3}$| |
Falomo et al. (2014) (QSO1) | |$42\%^{+3}_{-3}$| | |$37\%^{+3}_{-3}$| | |$21\%^{+3}_{-3}$| |
Cales et al. (2011) (QSO1) | |$24\%^{+9}_{-7}$| | |$72\%^{+5}_{-13}$| | |$4\%^{+8}_{-1.4}$| |
Greene et al. (2009) (QSO2) | |$27\%^{+19}_{-9}$| | |$73\%^{+9}_{-17}$| | |
Wylezalek et al. (2016) (QSO2) | |$10\%^{+11}_{-4}$| | |$90\%^{+4}_{-11}$| | |
Inskip et al. (2010) (NLRG) | |$6\%^{+11}_{-3}$| | |$88\%^{+1}_{-17}$| | |$6\%^{+11}_{-3}$| |
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