Age constraints on island-arc submarine basalts from geomagnetic paleointensity

Earth, Planets and Space

Table 2 NRM demagnetization data

Sample	Specimen	L (mT)	H (mT)	MAD of ChRM (°)	MDF (mT)	Comment
HPD#997-R08	1	0.1	150	4.005	32.9	Unoriented, small chip
HPD#997-R08	2	0	150	3.479	40.5	Unoriented, small chip
HPD#997-R08	3	0	150	6.103	39.6	Unoriented, small chip
HPD#997-R09	1	55	150	1.209	67.4
HPD#997-R09	2	40	150	0.515	59.6
HPD#997-R09	3	40	150	0.448	53.8
HPD#997-R09	4	55	150	1.242	50.6
HPD#999-R10	1	25	150	1.636	20.2
HPD#999-R10	2	20	150	1.676	19.7
HPD#999-R10	3	30	150	2.754	21.7
HPD#999-R10	4	30	150	2.486	20.5
HPD#1004-R06	1	30	150	0.411	64.7
HPD#1004-R06	2	35	150	0.289	49.9
HPD#1004-R06	3	15	150	0.262	58.5
HPD#1000-R09	1	15	150	0.879	28.8
HPD#1000-R09	2	25	150	0.393	50.3
HPD#1000-R09	3	20	150	0.601	41
HPD#1000-R09	4	30	150	0.413	44.8
HPD#1000-R10	1	15	150	0.712	39.3
HPD#1000-R10	2	15	150	3.837	24.5
HPD#1000-R10	3	15	150	2.276	13.6
HPD#1000-R10	4	30	150	2.948	20.6

L lower field end for the PCA calculation. H higher field end for the PCA calculation, MAD maximum angular deviation, MDF median destructive field