| Name |
Format |
Description |
Link |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vy_sig_frac_0.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vy_sig_frac_50.dat |
|
9 |
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vy_50.dat |
|
9 |
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vx_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vx_ten_frac_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vy_ten_frac_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vx_tencluster_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vy_ten_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vx_ten_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vy_ten_frac_0.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vx_sig_frac_0.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vy_sig_frac_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vx_ten_frac_0.dat |
|
9 |
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing. |
https://gdr.openei.org/files/1082/vsp_Vx_nofrac.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vy_ten_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vy_ten_frac_0.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vy_tencluster_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vy_tencluster_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vx_ten_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vx_sig_frac_50.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vx_sig_frac_0.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using surficial seismic data with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vy_sig_frac_0.dat |
|
9 |
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%. |
https://gdr.openei.org/files/1082/vsp_Vx_100.dat |
|
9 |
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vy_0.dat |
|
9 |
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vx_0.dat |
|
9 |
Seismic modeling results in a non-fractured medium, using vertical seismic profiling (VSP) with 1m spacing. |
https://gdr.openei.org/files/1082/vsp_Vy_nofrac.dat |
|
9 |
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%. |
https://gdr.openei.org/files/1082/seis_Vy_100.dat |
|
9 |
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vx_50.dat |
|
9 |
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vx_0.dat |
|
9 |
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vy_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/seis_Vx_tencluster_frac_50_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing. |
https://gdr.openei.org/files/1082/seis_Vy_nofrac.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vy_ten_frac_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vx_ten_frac_50.dat |
|
9 |
Seismic modeling results in a non-fractured medium, using surficial geophones with 1m spacing. |
https://gdr.openei.org/files/1082/seis_Vx_nofrac.dat |
|
9 |
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vy_0.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/vsp_Vx_tencluster_frac_50_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vx_tencluster_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vx_tencluster_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results in a single-fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vx_sig_frac_50.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vx_ten_frac_0.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/vsp_Vy_tencluster_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vy_tencluster_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/seis_Vy_ten_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 100%. |
https://gdr.openei.org/files/1082/vsp_Vy_100.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/vsp_Vy_tencluster_frac_0_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/seis_Vx_tencluster_frac_0_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vx_ten_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vy_ten_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results using surficial geophones with 1m spacing and a CO2 saturation of 100%. |
https://gdr.openei.org/files/1082/seis_Vx_100.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/vsp_Vy_tencluster_frac_50_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/seis_Vy_tencluster_frac_0_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 50%. |
https://gdr.openei.org/files/1082/vsp_Vx_tencluster_frac_50_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 0%. |
https://gdr.openei.org/files/1082/seis_Vx_ten_frac_0_1m_spacing.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using vertical seismic profiling (VSP) with 1m spacing and a CO2 saturation of 0%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/vsp_Vx_tencluster_frac_0_1m_spacing_newgeometry.dat |
|
9 |
Seismic modeling results in fractured media (ten parallel fractures aligned), using surficial geophones with 1m spacing and a CO2 saturation of 50%. This model uses a a new source-receiver geometry setting. |
https://gdr.openei.org/files/1082/seis_Vy_tencluster_frac_50_1m_spacing_newgeometry.dat |