Source provenance
Badgley, C. & Tauxe, L. (1990). Paleomagnetic stratigraphy and time in sediments: studies in alluvial Siwalik rocks of Pakistan. Journal of Geology, 98, 457-477.
Cited by 2 units (2 published) · 0 field-level citations · 2 revision notes.
Reviewer-supplied. High-resolution magnetostratigraphy of the Dhok Pathan and Chinji Formations documenting strong lateral variability in sediment-accumulation rate and time-transgressive sandstone/paleosol units - corroborating the Middle Siwalik magnetostratigraphic framework and cautioning that formational boundaries are diachronous.
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Units citing this source
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- Age: Badgley & Tauxe (1990): lateral tracing of reversal boundaries in the Chinji Formation shows secular change in sediment-accumulation rate and time-transgressive sandstone units, so the Chinji–Nagri lithofacies boundary is diachronous — individual strata span more time laterally than in a single vertical transect.
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- Age: Badgley & Tauxe (1990): dense transition-stratigraphy sampling of a magnetic reversal within the Dhok Pathan Formation reveals highly variable accumulation rates over 10^3–10^4 yr and time-transgressive paleosol and floodplain-marsh horizons, underscoring that the formation boundaries are diachronous.