Formation of corrensite, chlorite and chlorite‐mica stacks by replacement of detrital biotite in low‐grade pelitic rocks

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Abstract
Transmission and scanning electron microscopy were utilized to investigate the nature and mechanisms of alteration of abundant detrital biotite of volcanic origin and progressive modification of phyllosilicate aggregates in a prograde sequence of pelitic rocks (illite crystallinity index = 0.19–0.58d̀λ2θ) from the Gaspé Peninsula in Quebec.Detrital biotite has been diagenetically altered to form corrensite and chlorite through two mechanisms; (1) layer‐by‐layer replacement gave rise to interstratification of packets of layers and complex mixed layering via several kinds of layer transitions between biotite and chlorite, corrensite or smectite; (2) dissolution‐transport‐precipitation resulted in the formation of relatively coarse‐grained aggregates of randomly orientated, corrensite‐rich flakes and fine‐grained corrensite intergrown with chlorite and illite in the matrix.The data show that stacks consisting of alternating packets of trioctahedral and dioctahedral phyllosilicates originated during early diagenesis when lenticular fissures in strained altering biotite were filled by dioctahedral clays. Subsequent prograde evolution of dioctahedral clays occurred through deformation, dissolution and crystallization, and overgrowth. Illite evolved to muscovite, with K in part provided through biotite alteration, and corrensite/chlorite to homogeneous chlorite. The alteration of detrital biotite is closely related to the formation of titanite and magnetite in diagenetic rocks, and pyrite, calcite and anatase or rutile in the higher grade rocks.The observations demonstrate that detrital biotite of volcanic origin may be the principal precursor of chlorite in chlorite‐rich metapelites originating in marginal basins. The mineral parageneses suggest that the transitions from corrensite to chlorite and illite to muscovite may be a function of local chemistry and time.

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