Diamantes do rio Borrachudo, bacia do São Francisco (Tiros, MG): aspectos morfológicos e de dissolução
Luis Alberto de Deus BorgesI; Mario Luiz de Sá Carneiro ChavesII; Joachim KarfunkelIII
IGeologist of the Petrus Mineração Patos de Minas, Minas Gerais, Brasil. petrus@petrusminera.com
IIAssociate Professor Universidade Federal de Minas Gerais Instituto de Geociências Belo Horizonte - Minas Gerais - Brasil. mlschaves@gmail.com
IIIAssociate Professor Universidade Federal de Minas Gerais Instituto de Geociências Belo Horizonte - Minas Gerais - Brasil. jkarfunkel@yahoo.com
ABSTRACT
A representative set of diamonds from the Borrachudo River (114 stones) was described for the first time as to their physical characteristics, among them weight, morphology, dissolution figures, and abrasion. Most samples are low in weight (~51% less than 0.30 ct) and only ~3.5% are above 3.0 ct. However, considering the total weight, ~47% of it is concentrated in the range above 3 ct. On the other hand, there even occur diamonds with dozen of carats. The most common crystallographic forms are originated from the octahedral form by dissolution, although irregular shapes like chips and flats also occur. The diamonds show differences in form compared to their weight ranges; those up to 0.30 ct have various shapes; in the range of 0.31 to 1 ct the most common are octahedral forms and their descendants; and in stones larger than 1 ct chips and flats predominate. The general habitus of the crystals, identified by their final tetrahexahedroid shapes, chips and flats, corroborated by the dissolution figures, indicate that the diamond were submitted to strong dissolution in a magmatic environment. Residual hillocks and holes represent the final stage of dissolution. The study indicates that the abrasion by the fluvial transport was not expressive enough to cause mechanical wear, thus ca. 97% shows no sign of wear. This fact suggests a proximal source for most of these diamonds.
Keywords: Diamond, Borrachudo River, São Francisco Basin
RESUMO
Uma população representativa de diamantes do rio Borrachudo (114 cristais) é pela primeira vez descrita quanto às suas características físicas, envolvendo peso, morfologia, figuras de dissolução e abrasão. A maioria das amostras possui peso reduzido (~51% inferior a 0,30 ct) e apenas ~3,5% acima de 3,0 ct. No entanto, em relação ao peso total, ~47% concentra-se na faixa de peso acima de 3 ct, sendo observados, ainda, diamantes com dezenas de quilates. As formas cristalográficas mais comuns são oriundas da dissolução da forma original octaédrica, embora formas irregulares como chips e flats também ocorram. Os diamantes apresentam diferenciações quanto às suas formas em relação às faixas de peso; os com até 0,30 ct mostram-se em formas variadas; entre 0,31 a 1 ct ocorrem formas octaédricas e suas descendentes; e, nas amostras maiores que 1 ct, predominam os chips e flats. O habitus geral dos cristais, identificado pelas formas tetraedróides finais, chips e flats, juntamente com as figuras de dissolução, indicam que os diamantes sofreram uma forte dissolução no ambiente magmático. No estágio final do processo, são, ainda, observadas figuras de corrosão como hillocks residuais e buracos. O estudo da abrasão fluvial indica que o transporte não foi expressivo para causar desgaste mecânico, logo cerca de 97% não apresenta sinais abrasivos. Este fato sugere uma fonte proximal para a maioria desses diamantes.
Palavras chaves: Diamante, Rio Borrachudo, Bacia do São Francisco
1. Introduction
The Borrachudo River is a left margin tributary of the São Francisco River, flowing in NE-SW direction parallel to the Abaeté (west) and Indaiá (east) rivers, both also diamondiferous (Figure 1). Diamonds were discovered in the Abaeté River, considered the richest among the three, in the mid-eighteenth century by runaway slaves from the Diamantina District, which was at this time the main area of the country where the mineral was explored (Barbosa, 1991).
2. Regional geology and diamond deposits
The focused area is part of the "Western São Francisco Diamondiferous Province" (Chaves & Chambel, 2003), one of the four major diamond provinces of Minas Gerais. No detailed study of this region has been made, although it has been mapped recently at a 1:100,000 scale (Reis, 2011). The oldest rocks belong to the Canastra and Bambuí groups, of Neoproterozoic ages (Figure 1), consisting mostly of quartzites for the first group, and metasiltstones with interbedded limestones for the latter group, which were folded and metamorphosed during the Brasiliano orogenic cycle (0.65 to 0.50 Ga).
The covering sediments of the Precambrian rocks have been deposited mainly during the Cretaceous Era. The oldest deposits correspond to the Areado Group (Lower Cretaceous), consisting of thin grained sandstones with large cross stratifications, and the Mata da Corda Group (Upper Cretaceous) which consists of sandstones and volcanoclastic rocks. Local unconsolidated sandy sediments (Tertiary?) also occur, probably formed by the dismantlement of the underlying deposits. The important fracturing pattern observed, responsible for the SSW-NNE direction of major drainages, apparently follows a normal fault system that was originated from extensional events (Fuck & Pereira, 2005). The diamond deposits of this region and their possible source have been the subject of studies by some authors (e.g. Barbosa et al., 1970; Tompkins & Gonzaga, 1989; Read et al., 2004).
Alluvial diamond deposits occur in the Borrachudo River and some of its tributaries (Figure 1, featured on the right side). In the studied area, the deposits are related to three periods, all of them probably of Holocene Era (Reis, 2011). The oldest one occurs as alluvial terraces, elevated up to 20 m relative to the current channel of the river and consists of unconsolidated gravels with variable thickness up to 2 m. Paleochannels of younger eras occur on both banks of the river (about 2 m above its actual trough), whose remnants are up to 8 m thick (2-3 m of basal gravel and 30-35 m wide); these deposits are currently undergoing mining activity and its diamonds are the focus of this study (Figure 2A-B). The younger deposits are alluvial sediments of the riverbed.
3. Physical aspects of the diamonds from the Borrachudo River - Results
The physical characteristics of the diamonds are very important to understand their primary sources, to define different genetic "families", as well as to understand their primary paths, the surface distances from the source rock until its deposition site in the alluvium. Several authors have studied the morphology and dissolution figures of diamonds, using both descriptive and statistical methods in primary and secondary deposits (e.g. Svisero, 1971; Harris et al., 1975; Chaves, 1997; Martins, 2006), as well as by purely experimental methods (e.g. Orlov, 1977; Kosai & Arima, 2005; Khokhryakov & Pal'yanov, 2007).
The knowledge of the diamond transformation processes from their original form may indicate the fundamental conditions of formation of their host bodies, and the dissolution of the crystals in the ascent magma presents aspects other than those occurring in the river system. In the present study, the physical parameters are shown in four different interconnected parameters: characterization of crystal weight and morphological patterns, both indicating the transformation degree by dissolution; their dissolution figures, which show the relative stage of this process; and the abrasion, which is the final shape produced by mechanical wear during the fluvial transport.
Weight (ct)
The weight ranges were selected according to the general pattern observed in diamonds from the Western São Francisco Diamondiferous Province, according to the original proposal of Chaves & Chambel (2003). In the studied parcel, a numerical predominance of samples weighing up to 0.30 ct (~51%) occurs, followed by another range between 0.31 and 1.00 ct (~37%) (Figure 3A). The presence of some diamonds weighing over 20 ct was also detected. Thus, taking into consideration all weight categories, including isolated larger stones, this situation changes considerably, showing a significant percentage (~47%) concentrated in the range heavier than 3 ct (Figure 3B).
The most common growth forms of the studied diamonds are the cube {100}, octahedron {111}, and rhombic dodecahedron {110} (Figure 4). The crystals may often not have definite shapes (as chips and flats) due to disproportions in the growth given by different speeds along specific crystallographic axes. In general, the dissolution process naturally causes a gradual bulging of the crystal surfaces and thus new shapes are produced.
According to many authors (e.g. Kozai & Arima, 2005; Khokhryakov & Pal'yanov, 2007) the dissolution figures develop in a sequential line, where three stages in the process are recognized: (1) initial stage, where negative or positive trigons appear, as well as hillocks in blocks or pseudopyramids; (2) intermediate stage, showing secondary cleavage, residual hillocks, lamination and undulation lines; and (3) final stage, with the formation of holes and patina like.
Among the dissolution figures, hillocks in blocks and pseudopyramids predominate, followed by positive trigons and secondary cleavage, mainly in chip type diamonds. Another observation is that in the octahedron the morphological evolution is accompanied by dissolution figures in their respective dissolution stages (Table 3).
Abrasion is the mechanical wear process given by fluvial transport. In the studied population, diamonds of the Borrachudo alluvium without wear largely predominate (97.4%). Only three samples (2.6%) showed some small signs of wear. This means negligible transport, and therefore the source area was relatively near (Figure 8).
4. Concluding remarks
The origin of diamonds from the region related to the Abaeté, Borrachudo, and Indaiá rivers has always been a conundrum. Unlike the adjacent province to the southwest (Alto Paranaiba Province), where dozens of kimberlite intrusions in Coromandel and surrounding municipalities are known (although a real connection between these intrusions and mineralized alluvial deposits has never been established), in the Western São Francisco Diamondiferous Province certain problems are added.
In the headwater areas of these three rivers, extensive regions of volcanic and volcanoclastic rocks of the Mata da Corda Group (Upper Cretaceous) occur, hiding possible kimberlite intrusions. However, the presence of tributaries with diamond occurrences (as in the Grande, Águas Claras, and Carrão streams - Figure 1 detail) is also known. Such streams do not emanate from the headwaters of the Borrachudo River, indicating the possible existence of more than one area of primary mineralizing rock sources, not discarding the possibility of Cretaceous deposit reworking. Similar to what occurs in other alluvial systems in the region, such as in the Abaeté and Sono rivers (Chambel & Chaves, 2003), it is probable that a mixture of diamonds from different sources occur.
The weight pattern showed that most of the parcel is below 0.30 ct, although larger samples are also found, in the shape of chips or flats. Thus, the study characterized two distinct families identified by: (1) well-formed crystals, always from octahedral shapes and its descendants, and (2) larger size chips and flat crystals. The morphology associated with the dissolution figures indicates that they have suffered intense alteration into the kimberlite (Tappert & Tappert, 2011), and that some of these features still suffered final corrosive attacks, resulting in holes and "patina" in the surface. The diamonds have not been subjected to abrasion, and the existence of chips with sharp edges indicate that the transport was slightly significant, reinforcing the idea of a possible proximal source for majority of the studied parcel.
5. Acknowledgements
The first author thanks the IGC/UFMG, where he finalizes his Master's Thesis. M. Chaves thanks CNPq for granting the research productivity scholarship and the facilities granted by Petrus Mining Co.
6. References
BARBOSA, O. Diamante no Brasil - histórico, prospecção e lavra. Rio de Janeiro: CPRM Editora, 1991. 136p.
Fonte: CPRM
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