
Figure 1.
Location of lamprophyres within the simplified geological map of WKF (modified after Nayak & Kudari, 1999) and disposition of various rare alkaline rocks. Lamprophyre outcrop abbreviations: KKL, Korrakodu (Raghuvanshi et al., 2019); SPL, Sivarampet (Khan et al., 2019; Phani et al., 2018); KGL, Kalagalla (Phani et al., 2020); MDL, Mudigubba (Pandey et al., 2017a); UKL, Udiripikonda (Pandey et al., 2017b); KUL, Khaderpet (Smith et al., 2013); P8, pipe 8 of Lattavaram (Phani, 2019). Alkali syenites (Suresh et al., 2010): Cc, Chintalacheruvu; Dn, Dancherla; Dp, Danduvaripalli; Vd, Vannedoddi; Pd, Pedavaduguru; Rp, Reddypalli; Yp, Yeguvapalli. Syenite- Gs- Golla (Phani et al., 2021); WKF, Wajrakarur Kimberlite Field.

Figure 2.
Field photographs of lamprophyres of WKF. (a) Korrakodu (Raghuvanshi et al., 2019), (b) Kadiri (Pandey et al., 2018), (c) Sivarampet, (d) Kalagalla, (e) Udiripikonda (Pandey et al., 2017a, 2017b), (f) Khaderpet, (g) Mudigubba, (h) Pipe-8 (Lattavaram). See text for photo sources. WKF, Wajrakarur Kimberlite Field.
Table 1.
Some salient features of lamprophyres of WKF and data sources used in this study.
| Location | Outcrop | Mineral assemblage | Rock type | Reference |
|---|---|---|---|---|
| Korrakodu (KKL) | Dike | Dark mica (60%–70%) within groundmass of feldspars, sphene, apatite, carbonates, and zircon | Kersantite | Raghuvanshi et al. (2019) |
| Kadiri (KDL) | Dike | Amphibole (magnesio-hornblende), biotite and feldspar phenocrysts in groundmass of epidote, titanite and apatite | Spessartite | Pandey et al. (2018) |
| Sivarampet (SPL) | Dike | Pyroxenes, olivine and feldspar in groundmass of mica, ilmenite and secondary amphibole carbonate and chlorite | Kersantite | Phani et al. (2018), Khan et al. (2019), Pankaj et al. (2020) |
| Kalagalla (KGL) | Dike | Phlogopite-biotite, feldspar, amphiboles in fine grained felspathic pyroxene groundmass | Spessartite | Phani et al. (2020) |
| Udiripikonda (UKL) | Dike | Clinopyroxene megacrysts in olivine, mica in feldspathic groundmass | Kersantite | Pandey et al. (2017a, 2017b) |
| Khaderpet (KUL) | Plug | Olivine pseudomorphs altered to calcite or saponite, fine titanite in a saponite-carbonate or serpentine matrix. rare magnesiochromite with titanite rims | Ultramafic lamprophyre | Smith et al. (2013) |
| Mudigubba (MGL) | Dike | Amphibole, clinopyroxene, sphene, feldspar (albitised) | Spessartite | Pandey et al. (2017a, 2017b) |
| Lattavaram (P-8) | Pipe | Olivine, serpentinised olivine pseudomorphs, phlogopite, Cr-diopside, pyrope, chromite, ilmenite within groundmass of same composition | Ultramafic lamprophyre | Dongre et al. (2017) |
Table 2.
Geochemical data of lamprophyres of WKF in comparison with Jharia lamprophyre.
| 2a. Representative major oxide compositions. | |||||||||
|---|---|---|---|---|---|---|---|---|---|
| KKL | KDL | SPL | KGL | UKL | KUL | MGL | P8 | Jharia | |
| SiO2 | 46.74 | 53.71 | 47.32 | 42.8 | 45.1 | 47.4 | 52.72 | 41.95 | 44.5 |
| TiO2 | 1.8 | 0.9 | 2.37 | 2.18 | 2.38 | 2.66 | 0.76 | 1.3 | 4.81 |
| Al2O3 | 17.64 | 12.24 | 13.94 | 9.02 | 14.19 | 7.51 | 9.14 | 5.18 | 8.38 |
| Fe2O3 | 8.52 | 10.32 | 9.89 | 16 | 11.27 | 8.47 | 7.05 | 0.1 | |
| MnO | 0.143 | 0.17 | 0.13 | 0.18 | 0.17 | 0.23 | 0.18 | 0.1 | 0.13 |
| MgO | 3.12 | 8.35 | 8 | 7.5 | 7.43 | 13.80 | 11.15 | 19.33 | 8.18 |
| CaO | 6.62 | 8.6 | 8.53 | 8.35 | 8.81 | 11.40 | 12 | 8.63 | 6.85 |
| Na2O | 3.32 | 2.49 | 3.1 | 1.1 | 2.1 | 1.43 | 2.21 | 0.35 | 0.33 |
| K2O | 6.63 | 1.31 | 3.09 | 3.73 | 4.73 | 0.83 | 1.13 | 0.57 | 5.52 |
| P2O5 | 0.95 | 0.28 | 0.48 | 0.43 | 0.67 | 0.28 | 0.37 | 0.3 | 1.6 |
| LoI | 3.42 | 1.52 | 2.7 | 8.54 | 2.37 | 10.9 | 1.58 | 14.5 | 10.88 |
| Total | 98.9 | 99.9 | 99.58 | 99.83 | 99.22 | 96.45 | 99.71 | 99.46 | 98.9 |
| Mg# | 63 | 60.2 | 58.24 | 77.4 | 62.39 | 71.5 | 76.8 | 84.5 | 62 |
| 2b. Selected cationic wt.% and trace element concentrations in ppm | |||||||||
|---|---|---|---|---|---|---|---|---|---|
| Location | Sample | Al | Fe | Ti | K | Na | Y | Ta | Sc |
| Karraokodu | KR1 | 9.33 | 6.62 | 1.08 | 5.5 | 1.64 | 22 | 6.2 | 9 |
| Karraokodu | KR2 | 9.55 | 6.08 | 1.08 | 5.41 | 1.87 | 22 | 6.1 | 9 |
| Karraokodu | KR3 | 9.16 | 6.63 | 1.08 | 5.52 | 1.57 | 4 | 6.3 | 9 |
| Karraokodu | KR4 | 9.49 | 6.6 | 1.02 | 5.42 | 1.59 | 25 | 6.3 | 7 |
| Kadiri | KD1 | 6.48 | 8.02 | 0.54 | 1.09 | 1.36 | 16 | 0.3 | 30 |
| Kadiri | KD2 | 6.48 | 7.51 | 0.45 | 1.79 | 2.35 | 15 | 0.3 | 29 |
| Kadiri | KD3 | 7.76 | 5.89 | 0.35 | 1.7 | 1.83 | 12 | 0.4 | 21 |
| Kadiri | KD4 | 7.31 | 6.96 | 0.47 | 1.57 | 1.40 | 15 | 0.3 | 25 |
| Sivarampet | SP1 | 6.77 | 7.07 | 0.97 | 2.97 | 1.40 | 22.33 | 2.12 | 15.82 |
| Sivarampet | SP2 | 6.19 | 6.74 | 1.02 | 2.82 | 1.31 | 24.5 | 2.32 | 13.2 |
| Sivarampet | SP3 | 6.99 | 7.79 | 0.9 | 2.66 | 1.42 | 25.3 | 2.34 | 14.45 |
| Sivarampet | SP4 | 6.78 | 7.16 | 0.97 | 3 | 1.56 | 22.33 | 2.12 | 14.82 |
| Kalagalla | KL1 | 4.77 | 8.24 | 0.71 | 2.27 | 0.82 | 17.3 | 2.01 | 17.09 |
| Kalagalla | KL2 | 6.25 | 7.38 | 0.72 | 2.16 | 0.67 | 12.5 | 1.89 | 16.4 |
| Kalagalla | KL3 | 6.46 | 8.56 | 0.72 | 2.49 | 0.66 | 15.7 | 1.94 | 15.8 |
| Kalagalla | KL4 | 5.45 | 8.21 | 0.84 | 2.15 | 1.29 | 17.04 | 2.04 | 15.5 |
| Udiripikonda | UD1 | 7.51 | 5.96 | 1.42 | 3.93 | 1.56 | 25 | 7.51 | 5.96 |
| Udiripikonda | UD2 | 7.07 | 5.95 | 1.37 | 3.96 | 1.27 | 23 | 7.07 | 5.95 |
| Udiripikonda | UD3 | 7.59 | 6.27 | 1.47 | 3.83 | 1.66 | 24 | 7.59 | 6.27 |
| Udiripikonda | UD4 | 7.62 | 3.15 | 1.44 | 3.46 | 2.08 | 25 | 7.62 | 3.15 |
| Khaderpet | KH1 | 0.68 | 2.74 | 0.4 | 0.68 | 0.31 | 9.15 | 1.3 | 6 |
| Khaderpet | KH2 | 0.78 | 2.74 | 0.33 | 0.78 | 0.53 | 9.65 | 1.3 | 8 |
| Khaderpet | KH3 | 0.8 | 2.78 | 0.41 | 0.8 | 0.37 | 10.9 | 2 | 8 |
| Khaderpet | KH4 | 1.11 | 2.66 | 0.32 | 1.11 | 0.74 | 13.8 | 1.8 | 8 |
| Mudigubba | MD1 | 4.84 | 8.47 | 0.46 | 0.41 | 1.63 | 16 | 0.1 | 54 |
| Mudigubba | MD2 | 5.13 | 7.49 | 0.4 | 0.65 | 1.87 | 15 | 0.1 | 50 |
| Mudigubba | MD3 | 4.4 | 7.6 | 0.4 | 0.38 | 1.59 | 17 | 0.1 | 56 |
| Mudigubba | MD4 | 4.1 | 7.66 | 0.41 | 0.47 | 1.57 | 17 | 0.1 | 55 |
| Pipe 8 | LV1 | 2.74 | 5.48 | 0.78 | 0.47 | 0.26 | 8.88 | 4.86 | 8.42 |
| Pipe 8 | LV2 | 2.75 | 5.79 | 0.82 | 0.5 | 0.33 | 9.7 | 5 | 10 |
| Pipe 8 | LV3 | 2.72 | 6.09 | 0.81 | 0.49 | 0.24 | 9.6 | 5.6 | 10 |
| Pipe 8 | LV4 | 2.7 | 5.87 | 0.08 | 0.48 | 0.33 | 10.2 | 4.9 | 10 |
| Jharia | JH1 | 4 | 8.24 | 3.58 | 4.31 | 0.69 | 41 | 11.4 | 21 |
| Jharia | JH2 | 2.6 | 7.66 | 1.97 | 3.42 | 0.19 | 26 | 0 | 11 |
| Jharia | JH3 | 3.46 | 7.32 | 2.94 | 4.01 | 0.5 | 35 | 7.01 | 40 |
| Jharia | JH4 | 3.66 | 7.31 | 3.47 | 3.92 | 0.56 | 40 | 0 | 24 |
[i] See Table 1 for data sources.

Figure 3.
Geochemical diagrams plotted using cationic wt.% (Ilupin & Lutz, 1971; Ilupin et al., 1974). (a) K vs Al diagram, (b) Ti vs K variation diagram, (c) Ti vs Al diagram, (d) K vs Fe diagram. Data used for comparison: Wajrakarur diamondiferous kimberlites (Phani & Raju, 2017), Narayanpet barren kimberlites (Dongre and Chalapathi Rao, 2012), Wawa diamondiferous lamprophyre (Lefebvre et al., 2005).

Figure 4.
Geochemical diagrams showing diamondiferous character of WKF lamprophyres. (a) Ta vs Sc variation diagram (Kaminsky et al., 2005) showing lamprophyres in comparison with other rock types. (b) Fe2O3 (wt.%) vs Y (ppm) diagram showing distinction between diamondiferous (prospective) and barren (non-prospective) kimberlites (Birkett et al., 2004). (c) Bivariant diagram between DG and TiO2 (wt.%) for lamprophyre samples of WKF showing inverse relation. Data for WKF kimberlites from Phani (2019). DG, diamond grade; WKF, Wajrakarur Kimberlite Field.
Table 3.
Summary of certain DIMs in lamprophyres in comparison with kimberlites and lamproites of WKF.
| Locality | CHR | CrDi | ILM | GRT | OLV | SPN | TTN | DIA |
|---|---|---|---|---|---|---|---|---|
| Lamprophyresa | ||||||||
| Korrakodu (KKL) | ||||||||
| Kadiri (KDL) | ||||||||
| Sivarampet (SPL) | X | X | X | |||||
| Kalagalla (KGL) | X | |||||||
| Udiripikonda (UKL) | X | X | X | |||||
| Khaderpet (KUL) | X | X | X | X | X | X | X | |
| Mudigubba (MGL) | X | |||||||
| Lattavaram (P-8) | X | X | X | X | X | X | ||
| Kimberlites and lamproitesc | ||||||||
| Muligiripalli (P-5) | X | X | X | X | X | X | X | X |
| Tummatapalli (P-13) | X | X | X | X | X | X | X | |
| Pennahobilam (P-16) | X | X | X | X | X | X | X | |
| Pennahobilam (P-17)e | X | X | X | X | X | X | X | |
| Lattavaram (P-4) | X | X | X | X | X | X | X | X |
| Venkatampalli (P-7) | X | X | X | X | X | X | X | X |
| Timmasamudram (TK-4)b | X | X | X | X | X | X | X | X |
| Chigicherla (CC-5) | X | X | X | X | X | X | X | X |
| Brahmanapalli (B1)d | X | X | X | X | X | X | X | X |
Table 4.
TiO2 and DG values of lamprophyres of WKF in comparison with kimberlites.
| Location | DG | TiO2 |
|---|---|---|
| Karraokodu | 1.85 | 1.80 |
| Karraokodu | 1.7 | 1.805 |
| Karraokodu | 1.86 | 1.81 |
| Karraokodu | 1.95 | 1.71 |
| Kadiri | 5.16 | 0.9 |
| Kadiri | 5.82 | 0.75 |
| Kadiri | 5.66 | 0.59 |
| Kadiri | 5.01 | 0.79 |
| Sivarampet | 2.43 | 1.62 |
| Sivarampet | 2.26 | 1.7 |
| Sivarampet | 2.87 | 1.5 |
| Sivarampet | 2.47 | 1.79 |
| Kalagalla | 4.25 | 1.18 |
| Kalagalla | 3.63 | 1.2 |
| Kalagalla | 4.06 | 1.2 |
| Kalagalla | 3.43 | 1.4 |
| Udiripikonda | 1.36 | 2.38 |
| Udiripikonda | 1.43 | 2.28 |
| Udiripikonda | 1.37 | 2.45 |
| Udiripikonda | 0.75 | 2.41 |
| Khaderpet | 7.35 | 0.66 |
| Khaderpet | 7.39 | 0.55 |
| Khaderpet | 6.3 | 0.68 |
| Khaderpet | 5.9 | 0.53 |
| Mudigubba | 7.08 | 0.76 |
| Mudigubba | 7.10 | 0.66 |
| Mudigubba | 7.65 | 0.66 |
| Mudigubba | 7.46 | 0.69 |
| Pipe 8 | 3.74 | 1.3 |
| Pipe 8 | 3.69 | 1.36 |
| Pipe 8 | 3.93 | 1.35 |
| Pipe 8 | 3.94 | 0.133 |
| Jharia | 0.77 | 5.97 |
| Jharia | 1.52 | 3.28 |
| Jharia | 0.88 | 4.91 |
| Jharia | 0.74 | 5.79 |
| WKF Kimberlitesa | ||
| Pipe-3 | 7.54 | 1.58 |
| Pipe-4 | 7.37 | 1.56 |
| Pipe-5 | 2.73 | 5.36 |
| Pipe-7 | 10.68 | 0.79 |
| Pipe-9 | 9.8 | 0.71 |
| Pipe-10 | 6.62 | 2.2 |
| Pipe-11 | 7.48 | 1.27 |
| Pipe-13 | 1.82 | 6.62 |
| Pipe-16b | 1.7 | 4.5 |